GRAIN AND FORAGE LEGUME YIELDS, WITH OR
WITHOUT INTERCROPPING
AND THE EFFECT OF LEUCAENA GREEN LEAF
MANURING
ON NITROGEN ECONOMY OF CORN
A DISSERTATION SUBMITTED TO THE GRADUATE
DIVISION OF THE
UNIVERSITY OF HAWAII IN PARTIAL FULFILLMENT
OF THE REQUIREMENTS FOR THE DEGREE OF
DOCTOR OF PHILOSOPHY
IN
AGRONOMY AND SOIL SCIENCE
AUGUST 1984
BY
Shiva Kumar Chaudhary
Dissertation Committee
A. Sheldon Whitney, Chairman
Peter P. Rotar
James A. Silva
Yoshinori Kanehiro
Douglas Friend
We certify that we have
read this dissertation and that in our opinion it is satisfactory in scope and
quality as a dissertation for the degree of Doctor of Philosophy in Agronomy
and Soil Science.
|
ACKNOWLEDGEMENT
The author wishes to
express his whole-hearted appreciation to Drs. A. S. Whitney and P. P. Rotar or
their guidance, advice, and encouragement in
bringing this long-term effort to a successful
conclusion. The author is
indebted to Dr. James A. Silva for his valuable suggestions especially in
statistical analysis and review of the manuscript and to Drs. Y. Kanehiro and
D. Friend for serving on his advisory committee and reviewing the manuscript.
The author is indebted to
and wishes to express his appreciation to the Department of Agronomy and Soil
Science and the NifTAL Project for their continued support and without whose
financial assistance this work would
not have been possible.
His gratitude is extended
to the Farm Manager,
Mr. Herbert
Omizo, and the staff of the
Waimanalo Research Station, and Mr. Y. Oshiro and Mr. Y. Nakatani of Mauka
Campus for their support and assistance
provided during the entire experimental period. Thanks are also extended to Mr. Miguel
Alvarey and Mrs.
M. R. Reiss
for helping in typing the manuscript.
The author extends his
special thanks to his wife, Meera Chaudhary, for her unfailing support,
continued encouragement, and understanding. Thanks are also extended to his
daughters, Neetu and Reetu, for their understanding and patience in waiting
several years for their parents to return.
The author is grateful to his parents and other members of his family
for their encouragement and support.
ABSTRACT
Field experiments involving growing of two
grain legumes and two forage legumes with or without corn were conducted during
five consecutive seasons in a very fine, kaolinitic, isohyperthermic, Vertic
Haplustoll soil in Hawaii to evaluate the yield potentiality and N economy of
these Cropping Systems.
Grain legumes evaluated were mungbeans (Vigna
radiata) and soybeans (Glycine max).
Corn grain yields increased in intercrops as compared to the
grain yields in control plots of corn (no N application). The increases in intercropped corn grain
yields over grain yields in control plots were 158, 163, and 163% in season 1, and
181, 146, and 118% in season 3 in corn/determinate mungbeans,
corn/indeterminate mungbeans, and corn/soybean intercrops, respectively. Grain yields of mungbeans and soybeans were
slightly depressed in intercroppings as compared to their monocroppings.
Harvest indices and plant heights of intercropped corn and legume crops were
not significantly different than those of their monocrops.
Total biomass produced by corn/grain legume
intercropped plots (6.11 to 10.88 Mg ha-1) were much higher than the
biomass produced by control plots (3.08 to 4.33 Mg ha-1) of
corn. Total grain produced by
corn/grain legume intercroppings (1.58 to 3.45 Mg ha-1 ) were 4 to 6
times higher than the grain produced by control plots of corn (0.39 to 0.55 Mg
ha-1). LAI increased in
corn/legume intercrops as compared to their monocrops. LER values in these
intercropping systems were in the ranges of 1.9 to 2.2 in season 1 and 1.6 to
1.9 in season 3.
The grain yields and the plant heights of
corn following grain legume plots in season 2 and season 4 were comparable with
those of corn monocrops at 33 to 67 kg ha-1 levels of N application.
Nitrogen contributions from grain legumes to
associated corn crop were none in season 1 and 10 to 25 kg N ha-1 in
season 3. N contributions from legumes
to the following corn, however, were 40 to 58 kg N ha-1
in season 2 and 31 to 75 kg ha-1 in season 4. The residual N contribution to the following
corn was the highest by indeterminate mungbeans (58.0 to 75.0 kg N ha-l)
followed by soybeans (40.0 to 62.5 kg N ha-1) and determinate
mungbeans (35.0 to 47.0 kg N ha-1).
Nitrogen fixation by mungbeans and soybeans were not depressed in
intercroppings as compared to their monocroppings, except in soybeans in season
1 where soybeans were shaded by corn.
Forage legumes evaluated were leucaena (Leucaena
leucocephala) and desmodium (Desmodium intortum). Grain yields of corn intercropped with
leucaena were slightly higher than in control plots in all seasons
except season 2, where corn was shaded by
leuceana. Grain yields of corn
intercropped with leucaena were 128, 60, 122, and 102% of control plots of corn
in season 1 to 4, respectively. Grain
yields of corn intercropped with desmodium were slightly lower than the control
plots of corn in all seasons except season 4.
Grain yields of corn intercropped with desmodium were 72, 71,
91, and 118% of control plots of corn in season 1 to 4, respectively. In general, corn did better with leucaena
than with desmodium. However, corn
seemed to perform better with leucaena during summer and better with desmodium
during winter periods. Seasonal forage
yields of leucaena and desmodium were not different in intercrops than in their
monocrops. Total biomass produced by
corn/forage legume intercropped plots (4.5 to 17.0 Mg ha-1) were
much higher than the biomass produced by control plots (3.08 to 4.33 Mg ha-1)
of corn. LAI was higher in
intercropping than in the control plot of corn. Total LER values in corn/leucaena and corn/desmodium intercrops
were in the ranges of 1.40 to 2.10 and 1.60 to 1.81, respectively.
Nitrogen produced by leucaena was from 630 to
653 kg ha-1 yr-1 and by desmodium was from 508 to 608 kg
ha-1 yr-1. Total
N yields obtained from corn/leucaena intercroppings were 7 to 21 times and from
corn/desmodium intercroppings were 7 to 14 times as much as the N yields
obtained from die control plots of corn.
N contributions from forage legumes to associated corn were none in
season 1 and season 2, however, there was some N contribution from legume to
associated corn in season 3 and season 4 (19 to 30 kg N ha-1 from
leucaena and 9 to 17 kg N ha-1 for desmodium). Corn following forage legumes in season 5
received residual N of 21 to 31 kg ha-1 from leucaena plots and 23
to 30 kg ha-1 from desmodium plots.
In another field experiment, leucaena forage
was incorporated into soil as green manure for corn and the residual effects
were evaluated in the second season.
Corn grain yields obtained from the leucaena green manuring at the rates
of 47, 94, and 141 kg N ha-1 were equivalent to corn grain yields
obtained from the urea-N rates of 18, 35, and 58 kg N ha-1,
respectively. The efficiency of
leucaena green manure to increase corn grain yield as compared to urea-N
applications were 37 to 41%. The amount
of residual N from leucaena green manure to the following crop of corn were equivalent to urea-N application rate of
13 to 30 kg N ha-1.
Recoveries of N from urea-N were 39.4 to 47.0% and from leucaena-N were
26.3 to 30.5% in season 1. Recoveries of residual leucaena-N in season 2 were 5.0 to 7.1%. The total N recovered from the applied
leucaena green manure were 31.7 to 37.6% by the two crops of corn.
A pot experiment was
conducted where 15N-tagged mungbean plant materials, shoot, root,
and shoot + root, were applied to a wheat crop and a second crop of wheat was
grown to evaluate the residual 15N remaining. Total dry matter yields and total N uptake
by the first crop of wheat increased with increasing rates of mungbean-N. Total dry matter and total N yields by wheat
crop 1 obtained from the 100 kg N ha-1 rate of all sources of
mungbean-N were comparable with those from 33 kg ha-1 rate of
urea-N. Except the higher rates of
mungbean-N applied (at and above 100 kg N ha-1), the residual
effects from all other mungbean-N treatments were not different than the
control plot. In both the wheat crops,
straw overyielded the grain at all levels and from all sources of N
applied. In contrast, N uptake by grain
was always higher than that by straw of wheat.
Wheat N derived from
mungbean-N increased with increasing rates of mungbean-N applied and were
higher (10.9 to 70.4%) by the first crop of wheat and lower (5.4 to 43.5%) by
the second crop of wheat. Most of the
mungbean-N applied were recovered by the first crop of wheat (11.1 to 33.9%) and only less than 6% of the N was
recovered by the second crop of wheat.
Recoveries of N were higher from shoot than from root treatments. Of the
two methods used, the difference method overestimated the N recovery over the
isotopic method.
TABLE OF CONTENTS
ACKNOWLEDGEMENT
...........................................3
ABSTRACT
..................................................4
LIST OF TABLES
............................................11
LIST OF APPENDIX TABLES ...................................13
LIST OF FIGURES
...........................................14
LIST OF APPENDIX FIGURES
..................................16
CHAPTER I. INTRODUCTION
...................................17
CHAPTER II. REVIEW OF LITERATURE ..........................19
Terminology
..........................................19
Competition and Yield
Advantages
in Intercropping
...................................20
Nitrogen Transfer from
Legume to
Non-legume
.........................................27
Green Leaf Manuring
..................................35
The Use of 15N-Labeled
Fertilizers ................... 40
Evaluation of
Intercropping
Experiments
........................................43
CHAPTER III. GRAIN LEGUMES WITH OR WITHOUT
INTERCROPPING WITH CORN (Zea
mays L.) ................47
INTRODUCTION
.........................................47
MATERIALS AND METHODS
................................49
Removal of Available N
from Soil .....................49
Fertilization
........................................50
Planting of the
Experiment ...........................50
Weed and Insect Control
..............................51
Harvesting
...........................................51
Plant Height,
Number of Pods, per
Plant and LAI ......................................54
Nitrogen Fixation
....................................54
Dry Matter Yield
.....................................54
Nitrogen Content
.....................................54
Nitrogen Recovery
....................................55
Evaluation
...........................................55
RESULTS AND DISCUSSION
................................56
Performance of Corn in
Intercropping ..................56
Performance of Grain
Legume in
Intercropping .......................................62
Total Performance in
Intercropping ....................66
Corn Following Grain
Legumes ..........................70
Environmental Effects
.................................77
Nitrogen Yield and
Transfer ...........................79
N Recovery from Urea .................................86
Soil Nitrogen
.........................................90
Effects on Nitrogen
Fixation ..........................90
SUMMARY AND CONCLUSIONS
.................................95
CHAPTER IV. FORAGE LEGUMES WITH OR WITHOUT INTERCROPPING
WITH CORN (Zea mays
L.) ............................99
INTRODUCTION
.......................................99
MATERIALS AND METHODS
.................................100
Planting
..............................................101
Weed and Insect Control
...............................102
Harvesting
............................................102
Plant Height and LAI
..................................103
Dry Matter Yield
......................................103
Nitrogen Contents
.....................................103
Evaluation
............................................104
RESULTS AND DISCUSSION
................................104
Performance of Corn in
Intercropping ..................104
Performance of Forage
Legumes .........................110
Total Performance in
Intercropping ....................116
N Yields and Transfer
.................................119
Performance of Corn
Following Forage
Legumes
.............................................123
SUMMARY AND CONCLUSIONS
...............................125
CHAPTER V. EVALUATION OF LEUCAENA (Leucaena Leucocephala
(Lam.) de Wit) AS A GREEN
LEAF MANURE
FOR CORN
(Zea mays L.)
..............................................132
INTRODUCTION .......................................132
MATERIALS AND METHODS
.................................133
Treatments
............................................133
Planting
..............................................134
Observations
..........................................135
Evaluation
............................................135
RESULTS AND DISCUSSION
................................136
Performance of Corn in
Season 1 .......................136
Performance of Corn in
Season 2 .......................138
Nitrogen Recovery .....................................145
Correlations ..........................................148
SUMMARY AND CONCLUSIONS
...............................148
CHAPTER VI. NITROGEN UPTAKE BY WHEAT CROPS FROM
15N-LABELED LEGUME PLANT
MATERIALS .....................153
INTRODUCTION
..........................................153
MATERIALS AND METHODS
.................................154
Tagging of Mungbeans
..................................155
Treatments
............................................155
Planting of Wheat
.....................................156
Harvesting
............................................156
Evaluation
............................................158
RESULTS AND DISCUSSION
................................159
Yield of Wheat Crop 1
.................................159
Nitrogen Uptake by Wheat
Crop 1 .......................161
Yields of Wheat Crop 2
................................165
Nitrogen Uptake by Wheat
Crop 2 .......................165
Nitrogen Recovery by Wheat
............................168
SUMMARY AND CONCLUSIONS
...............................176
APPENDIX TABLES
.............................................178
APPENDIX FIGURES
............................................189
LITERATURE CITED
............................................205
LIST OF TABLES
Table page
3.1 Sequence of crop
combinations grown in four
consecutive seasons
..................................52
3.2 Spacing, plant
density, planting and harvesting
dates, and growing
periods of crops ..................53
3.3 Corn grain
yields in intercrops and percent
increase over the control
plots ......................60
3.4 Harvest indices
of corn in seasons 1 and 3 ...........61
3.5 Plant height,
number of pods per plant
and
harvest indices of two
grain legumes .................65
3.6 Grain yields of
corn and legume intercrops ...........69
3.7 Leaf area
indices of corn and legumes
in season 1
..........................................71
3.8 Land equivalent
ratios in corn/grain
legumes intercrops
...................................72
3.9 Grain and dry
matter yields of corn
following grain legumes
..............................74
3.10 Harvest indices
and plant heights of
corn in seasons 2 and 4
..............................76
3.11 Percent N in
plant tissues of grain
legumes in seasons 1 and
3 ...........................84
3.12 Percent N in
corn ear leaves at 50% silking
in seasons 1 through 4
...............................85
3.13 Estimated
amount of N contributed to corn by
grain legs based on N
uptake by corn from
applied urea-N
.......................................89
3.14 Percent N
recovery from urea fertilizer ..............91
3.15 Nitrogenase
acitivity in legumes in
seasons 1 and 3
......................................93
3.16 Correlation
coefficients for the relationships
between variables related
to N2 fixation .............94
4.1 Percent change
in grain yields, of corn
intercropped with forage
legumes
compared to control plots
(monocropped
corn without N)
.......................................108
4.2 Harvest indices
and plant heights of corn in monocrops
compared to intercrops
with forage legumes ............109
4.3 Dry matter
accumulation of leucaena and
desmodium during their
growing period .................113
4.4 Leaf area
indices of corn and forage
legumes in season 1
...................................118
4.5 Land equivalent
ratios in corn/forage
legumes
...............................................120
4.6 Correlation
coefficients for the relationships
among dry matter yield, N
yield and % N in
leucaena and desmodium
................................124
4.7 Performance of
corn following forage
legumes in season 5
...................................127
5.1 Performance of
corn with leucaena
green manuring in season
1 ............................137
5.2 N yield and
percent N in plant tissues
of corn in season 1
...................................140
5.3 Performance of
corn in season 2 (residual effects
of leucaena green manure
from season 1) ...............142
5.4 N yield and
percent N in plant tissues
of corn in season 2
...................................147
5.5 Percent N
recovery from leucaena green manure
and urea in season 1 and
season 2 .....................149
5.6 Correlation
matrix of several variables of
corn in seasons 1 and 2
...............................150
6.1 Treatments, rate
of N, and amount of urea and
plant materials applied
...............................157
6.2 Yield of wheat
crop 2 .................................166
6.3 Percent N in
plant tissues and N
uptake by wheat crop 2
................................169
6.4 Nitrogen
recovery by two crops of wheat
estimated by
different methods ........................175
LIST OF APPENDIX TABLES
Table page
1 Grain and dry
matter yields of corn and
grain legumes in seasons
1 and 3 ....................178
2 Seasonal total
dry matter yields
in all the crops
....................................179
3 Solar radiation,
temperature and rainfall during
the period of experiment
at Waimanalo Research
station in Hawaii
...................................180
4 Seasonal N
yields in all the crops ..................181
5 Grain yield of
corn intercropped with forage
legumes in seasons 1 through 4
......................182
6 Seasonal dry
matter, N yield, and percent N of
leucaena and desmodium
..............................183
7 Annual dry
matter, and N yields of leucaena and
desmodium during their
growing period ...............184
8 Nitrogen content
in soil before and after
planting in each season
.............................185
9 Yield of Wheat
crop 1 ...............................186
10 Percent N in
plant tissues and N
uptake by wheat crop 1 ..............................187
11 Atom % 15N
in plant tissues of
two crops of wheat
..................................188
LIST OF FIGURES
Figure
Page
3.1 Effects of urea N application on grain
yield of corn in seasons 1 and 3
..........................57
3.2
Dry matter yields of corn in monocrops
compared
to intercrops in seasons 1 and 3
..........................58
3.3 Plant heights of corn in monocropped compared
to
intercropped in seasons 1 and 3
...........................63
3.4
Dry matter yields of grain legumes
in seasons 1 and 3
........................................64
3.5
Total dry matter yields in corn/grain legume
intercrops (C=corn and L=legume)
..........................67
3.6
Effects of urea N application on grain
yields
of corn in seasons 2 and 4
................................75
3.7
Effects of environmental conditions
on corn grain yields
......................................78
3.8
Total N yields in seasons 1 and 3
.........................80
3.9
Nitrogen yields in sequential crops of
corn in seasons 2 and 4
...................................82
3.10 Percent N in corn ear leaves at 50% silking
at four levels of urea N application
......................87
3.11 Nitrogen uptake by corn at four levels
of urea N application
.....................................88
4.1 Effects of urea N application on grain
yield of corn in seasons 1 to 4 ....................106
4.2 Dry matter yields of corn in monocrops as
compared
to intercrops in seasons 1 and 4 ..........................107
4.3
Seasonal yields of leucaena and
desmodium in
intercrops as compared to monocrops
.......................111
4.4
Environmental effects on dry matter
yield and dry
matter accumulation of leucaena and desmodium
.............114
4.5
Total dry matter yields in monocrops of
corn
compared to corn/forage legume intercrops
.................117
4.6
Total N yields in monocrops of corn
compared
to corn/forage legume intercrops
..........................121
4.7
Effects of urea N application on grain
yield of corn in season 5
.................................126
4.8
Effects of urea N application on N
uptake of corn in season 5
...............................128
5.1
Effects of urea N application on grain
yield of corn in season 1
................................139
5.2
Effects of urea N application on N
uptake by corn in season 1
...............................141
5.3
Effects of urea N application on grain
yield of corn in season 2
................................144
5.4
Effects of urea N application on
N uptake by corn in season 2
.............................146
6.1
Wheat yield as affected by urea-N
and mungbean-N applications
..............................160
6.2
Relationship between urea-N application
and dry matter yield of wheat crop
.......................162
6.3
Nitrogen uptake by wheat crop 1 as
affected
by urea-N and mungbean-N applications
....................163
6.4
Relationship between urea-N application
and N uptake by wheat crop 1 .............................164
6.5
Relationship between urea-N application
and
dry matter yield of wheat crop 2
.........................167
6.6
Relationship between urea-N application
and N uptake by wheat crop 2
.............................170
6.7
Nitrogen derived by two crops of wheat
from
mungbean plant materials and soils
.......................172
LIST OF APPENDIX FIGURES
Figure
Page
1 Planting patterns of crops in: A)
monocrops,
and B) intercrops
.........................................189
2 Growth of soybeans in: A) monocrop, B)
intercrop
in season 1 (shaded), and C) intercrop in
season
3 (not shaded)
............................................192
3 Growth of determinate mungbeano as A)
monocrop and
B) intercrop, and of indeterminate mungbeans as
C) monocrop and D) intercrop
..............................195
4 Leucaena Shading corn in season 2
.........................198
5 Growth of leucaena A) monocrop and B)
interccop,
and desmodium
C) monocrop and D) intercrop ................199
6 Growth of wheat crop 1 at various rates of
A) urea-N, B) mungbean shoot-N, C) root-N,
and D) shoot + root-N applications
........................202
CHAPTER
I
INTRODUCTION
The shortage and ever
increasing prices of food commodities have put greater pressure on research
organizations to study the efficiency of farm inputs used for food
production. Increased crop production
is limited by several factors, including the high cost and short supply of industrial
fertilizers, particularly nitrogen.
Increasing price of nitrogenous-fertilizers, and the difficulties in
transportation and distribution, make them effectively unavailable to the small landholder.
Legumes hold great
potential as source’s of high protein food and feed, and have received considerable
attention from research organizations. Above all, because of their ability to
fix significant amounts of atmospheric nitrogen, legumes become more important
and offer an alternative for increasing nitrogen input in various cropping
systems and soil management practices.
Multiple cropping (or
polycropping) has been a long standing practice in many of the developing
countries. Polycropping systems include
both simultaneous and sequential mixed cropping and imply a more efficient use
of resources (space, soil fertility, moisture, solar radiation, and other
environmental growth factors) within the farmer’s socio-economic circumstances
to maximize yield with minimum risk, minimum input and maximum ecological
stability.
Legumes are frequently
grown with non-legumes in some form of polycropping systems. Legumes may contribute nitrogen to
associated non-legumes by releasing or excreting N from their roots or to succeeding non-legume
crops from the plant residues left in the soil. The inclusion of legumes in cropping systems thus has the
potential for improving the nitrogen economy of the whole system.
Corn is one of the major
cereal crops widely used in cereal/legume intercropping. The
choice of legumes in cropping systems depends on their compatibility with other
non-legume crops. Legumes differ in
their N fixing capacity and N requirements for their growth. It is therefore important to assess the
compatibility and the N contribution of several legumes to the corn crop in
order to develop a cropping system which may provide maximum N contribution
from legume to non-legume, and thereby greatly reduce the input of nitrogenous
fertilizers.
Legumes can also
contribute N to non-legumes, when used as an N source, in the form of green
manures. The use of legumes as green
manures has been in practice for a long time in many parts of the world. Green
manuring is the use of fresh plant material to modify soil conditions
with the objective of improving the soil as a medium for plant growth. Green plant material may be placed on the
soil surface as mulches or may be
incorporated into the soil, and all plants may be considered as green manures when they
are grown or harvested for this purpose.
The degree of N benefit from legumes
either intercropped with nonlegumes or used as green manures depends on the
amount of N remaining in either the
legume residues or in the legumes added into the soil. Not
all the organic N added
into the soil is mineralized or is readily available to the companion crop, therefore, it is
important to evaluate the proportion of the added N that is utilized.
The studies reported here represent an
attempt to a) compare the N contribution of two grain and two forage legumes to
a corn crop, b) examine the potential of leucaena foliage as a green manure to
corn, and c) determine the uptake of N by a cereal crop from the legume plant
residues with the use of 15N-labeled fertilizer.
CHAPTER
II
REVIEW
OF LITERATURE
Terminology
Legumes are frequently
grown with non-legumes in some form of polycropping system (intercropping,
relay cropping, mixed cropping or strip cropping). Intercropping is defined as the growing of two (or more) crops
simultaneously on the same area of ground.
Crops are usually grown simultaneously for a significant
part of their lifecycle, hence intercropping is distinguished from "relay
cropping" in which growing periods only briefly overlap. Crops are grown in separate rows in
intercropping, and any arrangement where there is irregular broadcasting or
mixing within the row is defined as "mixed cropping". In strip
cropping, two or more crops are grown simultaneously in different strips wide
enough to permit independent cultivation but narrow enough for the crops to
interact agronomically.
Several other terms are
used to describe various cropping systems; multiple cropping or polycropping is
defined as a cropping system in two or more crops are grown on the same field
in a year. Intercropping and sequential
cropping are forms of multiple cropping.
Sequential cropping is a system where two or more crops are grown in
sequence on the same field per year.
Several other related
terminologies commonly used in multiple cropping systems are sole cropping,
monoculture or monocropping, rotation cropping, cropping pattern, cropping systems,
and mixed farming. Sole cropping is the
growing of one crop variety in pure stands,
and is also called solid planting.
Monoculture is the repetitive growing of the same crop on the same
land. Rotation cropping is the
repetitive cultivation of an ordered succession of crops on the same land. A cropping pattern is the yearly sequence
and spatial arrangement of crops or of crops and fallow in a given area. A cropping system is the cropping patterns
used on a farm and their interaction with farm resources, other farm
enterprises, and available technology which determine their makeup. Mixed farming is the cropping systems which
involve the raising of crops, animals, and/or trees, and such systems are also
called farming systems.
Competition and Yield Advantages in Intercropping
Intercropping systems are more complex than
monoculture systems. There is both
inter - and intra - crop competition in intercropping systems in contrast to
only intra-crop competition in monocultures.
Allen et al. (l976), in a review of the literature, classified
interaction between two species populations as follows: a) commensalistic,
where the interaction between crop species has a positive net effect on one
species and no effect on the other species, b) amensalistic, where the
interaction between crop species has a negative net effect on one species and
no effect on the other species, c) monopolistic, where the interaction between
crop species has a positive net effect on one species a negative effect on the
other species, and d) inhibitory, where the interaction between crop species
has a net negative effect on all species.
Several other terms are
also used to describe the interaction between two species growing together
(Willey, 1979a). When the actual yield
of each species is less than expected it can be termed as "mutual
inhibition" and is rare in practice.
In the second situation, where the yield of each species is greater than
expected, it can be termed "mutual cooperation" and is not
unusual. In the third situation, where
one species yields less than expected and the other yields more,
it can be termed as "compensation" and is the commonest situation.
In general, there are
yield advantages in intercropping over monocropping. These yield advantages occur when: 1) the combined intercrop
yield exceeds the yield of the higher-yielding sole crop, 2) the intercropping
gives a full yield of a "main" crop plus some additional yield of a
second crop, and 3) where the combined intercrop yield exceeds a combined sole
crop yield (Willey, 1981).
Legumes are well known
for their important role in various cropping systems (Francis et al., 1975;
Dart and Krantz, 1977; Moomaw et al., 1977; Pinchinat, 1977). Intercropping of short-duration pulses with
pastures and field crops are very common in many parts of the world (Mahapatra
et al., 1975; Saxena and Yadav, 1975, Singh and Prasad, 1975; Singh and Singh,
1975). Various grass/legumes mixtures
in forage production are also widely practiced (Kretschmer et al., 1973; Keya,
1974; Kitamura and Nishimura, 1976).
Yields of both legume and
non-legume are of often reduced in intercropping as compared with yields when
they are grown alone (Dalal, 1974; Syarifuddin et al., 1974). Yields of legumes are usually more depressed than that of
non-legumes in intercropping (Agboola and Fayemi, 1971). Finlay (1974), using several legumes,
reported that reduction in yields on the intercropped legumes ranged from 18 to
43%.
Other reports (Roquib et
al., 1973; Ahmed, 1976; Fisher, 1977; Gunasena et al., 1978) have shown a
reduction on yield of legume but no effect on non-legume. Singh (1977) added 5 legumes to a crop of
sorghum and reported that the sorghum intercrop yield exceeded the sole crop
with all legumes: increases ranged from 8.4% with soybean to 34% with cowpea
for fodder. Remison (1978) reported a
stimulatory effect in corn and cowpea mixtures and an increase in relative
yield total in mixtures as compared to monocultures. The value of the total yield of both legume and non-legume
intercrop is almost always higher than that from either of the monocrops (Gomez
and Zandstra, 1976; Ahmed and Gunasena, 1979).
The yield depression in
one crop or both in intercroppinq system may be due to the competition effects
and shading of one crop by another (Willey, l979a). The yield potentiality in a legume/non-legume intercropping
depends on their growth patterns, nutritional requirements, and compatibility
of the crops involved (Willey, 1979a, 1979b).
Competition among plants
occurs for water, nutrients and light (Donald, 1963; Rhodes, 1970). In intercropping, plants may have top
competiton for light and root competition for nutrients including water or
both. Kitamura et al., (1981) using Desmodium
intortum and Setaria anceps studied
top competition between the two species.
When only top competition was
allowed, desmodium was a better competitor for light than setaria. But when only root competition was allowed,
the root growth of setaria was dominant over desmodium, and the growth of
desmodium was depressed. When both (top
and root) competition was allowed (the normal situation in legume-grass
mixtures), desmodium was a poor competitor.
When legumes and grasses are grown together, competition among plants
moderate the effects of environmental factors such as light (Stern and Donald,
1962), water, and soil nutrients (Blaser and Brady, 1950).
In general, shading
decreases the photosynthetic capacity of leaves (Woledge, 1978) and thereby
decreases the dry matter yield (Eriksen and Whitney, 1982). Wong and Wilson (1980) studied the effects
of shading on the growth and nitrogen content of green panicgrass and siratro
in pure and mixed swards. They reported
that shading increased the shoot yield of green panicgrass while shoot yield of
siratro decreased with shading.
Nitrogen accumulation in green panicgrass was markedly improved by
shading. Shaded green panicgrass had a
higher leaf area index, better distribution of leaf area with height, and lower
extinction coefficients. Individual
leaves of green panicgrass grown in shade had greater photosynthetic activity
than those grown in full sunlight, while shaded siratro had a lower leaf area
index and lower photosynthetic potential than in the full sunlight. They suggested that the better growth of
green panicgrass under shade might be due to improved N status of the plants
compared with those in full sun. N
uptake into the whole plant of green panicgrass was increased by up to 34 and 52% under 60 and
40% sunlight, respectively. Singh et
al.(1974) have also reported higher photosynthetic rates for leaves of Panicum
capillare grown at 70 and 50% light compared with full sun.
Mungbeans are a
convenient crop for intercropping as they nature in a short period of time and
thrive under a wide range of conditions. Agboola and Fayemi (1972) reported
that the yield of corn in
corn/mungbean
intercropping (3,080 kg ha-1) was significantly higher than the
yield in monocrop (l,790 kg ha-1).
Several other researchers (Gunasena et al., 1979; Das and Mathur, 1980;
Kalra and Gangwar, 1980; Miah and Carangal, 1980; Rathore et al.,
1980) reported that corn yield was higher in corn/mungbean intercropping than
that in a monocrop of corn.
In experiments involving
grain legumes intercropped with corn, no adverse effect of mungbeans was found
on the yields of corn but the mungbeans yields were decreased (Agboola and
Fayemi, 1971; Ahmed, 1976; Singh and Chand l980).
Ahmed (1976) used several
legumes intercropped with corn and reported that mungbean/corn intercropping
provided the highest economic return among the crops tested. Advantages of growing mungbeans as an
intercrop over monocrop have been observed with many crops: Corn (Yingchul,
1976; Gunasena et al., 1978; Ahmed and Gunasena, l979), sorghum and pearlmillet
(De et al., 1978; Singh et al., l978), sugarcane (Chandra, 1978) and sunflower
(Campos and Macaso, l976).
Growth habit or type of
mungbeans may also have influence on the yield potentiality when grown with
cereals. In soybeans, determinate type plants attain most of their growth
before flowering begins but indeterminate types continue to grow even after
flowering begins (Egli and Leggett, 1973).
Reproductive and vegetative development of indeterminate soybeans occurs
simultaneously over a longer time than determinate soybeans (Scott and Aldrich,
1970). Similar growth patterns may be
true for determinate and indeterminate types of mungbeans, and thus
indeterminate type mungbeans may have a longer reproductive period than
determinate ones. A longer reproductive
period is usually associated with higher yield in mungbeans (Kua et al., l970).
Soybeans are another grain legume widely used
in intercropping with non-legumes. Nair
et al. (1979) using soybeans, cowpeas, pigeon peas and groundnuts as intercrops
with corn in India, reported that soybeans were the most suitable in
intercropping among the legumes tested.
In a comparison of pure and mixed cultures of corn, rice,
soybeans and pigeon peas grown in various combinations, the advantages of
soybean/corn intercropping were most apparent (Chatterjee and Roquib,
1975).
Jagannathan et al. (1979) reported that the
cultivation of corn and soybeans in 1:2 and 1:1 ratios increased the yield of
corn grain equivalents compared with corn in pure stands. The corn grain protein content was increased
in the mixed stands in the 1:2 ratio.
The protein and oil contents in soybean seeds were not affected. Other experiments showed an increase in corn
yield when intercropped with soybeans over the monocrop (Narang et al., 1969;
Kalra and Gangwar, 1980; Rathore et al., 1980; Singh et al., 1980; Srivastava
et al., 1980).
Other experiments showed decrease in corn
yield when intercropped with soybean over the monocrops (Wong and Kalpage,
1976; Dalal, 1977; Cordero, 1978; Gunasena et
al., 1979; Singh and Chand,
1980). Cordero (1978) reported that
corn yield was 17% less when intercropped with soybeans. However, the leaf area duration of corn in corn/soybean
mixtures was twice as long as in the monoculture and the productivity of the
intercrop was 20 to 40% greater than when the crops were grown alone.
Most studies involving
corn/soybean intercrops indicated that corn yields were usually not
affected but the soybean yields decreased (Roquib et al., 1973; Ahmed, 1976;
Singh, 1977; Mohta and De, 1980; Chowdhury, 1981; Searle et al., 1981). Mohta
and De (1980) evaluated several systems of intercropping corn and sorghum with
soybeans. They reported that the corn
yields were not affected by intercropping with soybeans but sorghum yields were
reduced. Though the seed yield of
soybeans when intercropped was less than that of a monocrop, the combined grain
yield of the two crops grown as intercrop was more than the individual
components. Land equivalent ratio (LER)
increased to a maximum of 48 and 31% by intercropping corn and sorghum with
soybeans compared with the cereal monocrops.
Superiority of intercropping soybeans with cereals over monocrop has
also been demonstrated by other workers (Finlay, 1974; Beat 1977; Ibrahim et al., 1977).
Cordero and Mecollum (1979)
applied various levels of N in corn/soybean intercrops and reported that as the
rate of N application was increased, the corn yields increased and the soybean
yields decreased. With the increased
level of N, corn had better growth and was dominant over soybeans.
Leucaena leucocephala is a
perennial tree legume that has recently attracted much attention. Efforts have been made to study
corn/leucaena intercropping (Mendoza et al., 1975; Guevarra, 1976; IITA, 1979;
Rosa et al., 1980; Kang et al., 1981b; Mendoza et al., 1981).
Guevarra (1976) observed
no yield reduction in the yield of any crop in the corn/leucaena
intercropping. He reported that crude
protein yield in the corn/leucaena intercrop was 1.44 t ha-1, which
was twice the protein yield (0.75 t ha-l) of corn alone with a
nitrogen application of 75 kg N ha-1, and three times the protein
yield (0.47 t ha-l) of corn with no nitrogen application.
At the International
Institute of Tropical Agricultuce (IITA, 1979), intercropping of leucaena with corn,
and with corn and cassava was studied.
The corn yields in corn/cassava (3.1 t ha-1) and
corn/leucaena (2.8 t ha-1) were higher than the corn alone (2.5 t ha-1).
Corn yield in corn/leucaena/cassava (l.8 t ha-1) was lower than the
corn alone but the cassava yield in corn/leucaena/cassava intercropping (29.2 t
ha-1) was higher than the corn/cassava intercropping (20.2 t ha-1). This indicated that the joint effect of both
crops adversely affected corn. The
marked difference in cassava yields between corn/cassava and
corn/leucaena/cassava indicated a beneficial effect of leucaena. This experiment suggested that intercropping
of leucaena with corn and corn/cassava is a feasible recommendation for the
establishment of leucaena in cropping systems.
Rosa et al. (1980)
working on Leucaena/corn intercropping reported that leucaena decreased the
time of maturity of the corn crop, and increased
the ear length, ear diameter and grain yield of corn. Grain yields of corn were increased from 48.5 g/ plant in pure stand
to 69.9-74.4 g/ plant in intercropping.
Erosion on hills during heavy rains was greater in pure corn stands than
intercropped corn.
Desmodium intortum is another perennial legume of interest in the
tropics. Increases in forage yield and
crude protein yield/ha by inclusion of desmodium with grasses has been observed by several workers (Younge et al.,
1974; Whitney et al., 1967; Whitney and Green, 1969; Whitney, 1970). So far, only few studies have been made
where desmodium was grown with cereal
crops.
Nitrogen Transfer from Legume to Non-legume
The practice of intercropping a cereal and
legume is based on the hypothesis that the cereal can utilize nitrogen fixed by
the legume. The legume way increase the
supply of available nitrogen in the root medium, but it may also compete with
the non-legume for this nitrogen (Simpson, 1965). Most of the experiments have
shown that non-legume benefits more from the increase in nitrogen supply than
it suffers from competition by the legume, and there is a net transfer of
nitrogen to the non-legume (Walker et al., 1954; Bryan, 1962).
In general, legumes are weaker competitors
far mineral N than grasses (Henzell and Vallis, 1977). When legumes are substituted for non-legumes
on a soil where the N supply is limiting, the remaining non-legumes are able
to take up more mineral N per plant than they would in a pure stand of
non-legumes, which is termed as the "N-sparing effect" of
substituting nodulated legume for non-legume plants (Vallis et al., 1967).
In general, it is found that non-legume crops
are unlikely to benefit from associated legumes sown at the same time unless
the non-legume plants continue to take up N after the legume plants have begun
to senesce and die. Thus, it seems that there may be two opposing considerations
in the choice of the relative time of sowing legumes and non-legume crops in
mixture. If the legume is sown early it
may compete with the non-legume for soil mineral N but there could be an
opportunity later for rapid and effective transfer of N to the non-legume
companion crop. On the other hand, if
the legume is sown late, the non-legume will already have taken up soil mineral
N but there will be little or no opportunity for N transfer immediately and
some legume N may even be lost before another crop can use it (Henzell and
Vallis, 1977).
The non-legume may receive N fixed by a
legume while grown together (Henzell and Vallis, 1977; Whitney, 1977), and or
while grown after tile legume in rotation (Talleyrand et al., 1977; Lal et al.,
1978; Singh and Awasthi, 1978; Ahlawat et al., 1981). Two major pathways by which N may be transferred from legume to
non legume: 1. Above ground transfer including a) urine and dung of grazing
stock, b) leaching of nitrogenous compounds from leaves by rain, c) decay of
fallen leaves or other litter, and 2. Underground transfer including a) direct
excretion of nitrogenous compounds from legume root systems and use by
non-legume root system, and b) sloughing off and decay of nodule and root
tissue (Virtanen et al., 1937; Walker et al., 1954; Whitney and Kanehiro, 1967;
Scott, 1973).
Virtanen et al. (1937) conducted extensive
experiments which showed that leguminous plants were able to excrete N into the
substrate in which they were growing and that the N may be utilized by
associated non-leguminous plants.
Similar results showing N excretion were reported by other workers
(Wilson and Wyss, 1937; Wilson and Burton, 1938; Whitney and Kanehiro, 1967).
In grain legumes, some evidence of N
excretion was shown by Vest (1971) in experiments where non-nodulating
soybeans, grown in half and halt mixture with two nodulating cultivars, had
higher yields, higher percent protein and larger seed size than the
non-nodulating line grown in pure culture.
In another experiment, Burton et al. (l983),
growing nodulating and non-nodulating soybean isolines in pure and in mixed
cultures, reported that the average performance of the non-nodulated component
of the mixture was 38% greater than the average yield of the non-nodulated line
in pure cultures, indicating that non-nodulated isolines benefited from
nodulated isolines in mixed culture.
Singh et al. (1974) found that yield and percent N of non-nodulating
soybeans increased as the frequency of nodulating border rows increased,
indicating the N release from nodulated plants to non-nodulated plants.
Release of N from the legume and its transfer
to an associated non-legume is significant only when vigorous legume growth
occurs. This N transfer is more common
in perennial than in annual legumes (Whitney et al., 1976). Seasonal conditions such as long days, low
temperatures and shading seem to favor N excretion (Wilson and Wyss, 1937;
Wilson, 1940; Wyss and Wilson, 1941; Butler et al., 1959). Carbon/nitrogen ratios have also been reported as a governing factor in N
fixation and N excretion by legumes (Virtanen, 1947). Brief wilting has also been found to cause N excretion
(Katznelson et al., 1955).
Most of the experiments
indicated that the transfer of N from living root system of legumes is only a
small percentage of the total N fixed (Henzell, 1962; Simpson, 1965; Vallis et
al., 1967; Whitney and Kanehiro, 1967; Henzell et al., 1968). The amounts of N turnover
by the decomposition of sloughed nodules, root tissues and foliar residues are
probably more important than the direct transfer of N between the legumes and
non-legumes (Misra and Misra, 1975; Subbarao, 1975; Tiwari and Bisen, 1975;
Simpson, 1976; Henzell and Vallis, 1977; Vallis, 1978; Whitney, 1982).
The availability of N
from legume residues depends on the rate of the mineralization process. The proportion of N released during
decomposition of the residues in governed by the chemical of these residues, especially the N content, the manner
in which the residues are returned to the soil, and the environmental
conditions. The chemical composition of
legume residues depends to a large extent on the proportion of different plant parts and
their maturity (Henzell and Vallis, 1977).
Amounts of N returned to
the soil in the form of legume residues vary widely according to the legume
yield and whether or not it is utilized for grain, forage, grazing or green manure. N content in grain legume residues may be lower than that in pasture legumes (Henzell and Vallis,
1977). Henzell and Vallis (1977) reported a N-content
ranges of 3-5% in tops and 2-4%
in roots in some pastures legumes. Hanway and Weber (1971) recorded 2% N in the fallen leaves from a mature soybean
crop and 0.9% N in the stems and roots.
Plant residues containing more than 1.8% N usually mineralize N
immediately, and those with less than 1.2% N usually immobilize it temporarily
(Alexander, 1961).
Part of the N in legume residues quickly
becomes available for reuptake and the remaining N after the initial flush of
mineralization becomes available only very slowly for later crops (Henzell and
Vallis, 1977; Vallis, 1978).
Bartholomew (1965) estimated that about 60% of the N in legume residues
is likely to be mineralized in time for the following crop. The remainder is lost or is incorporated
into the soil organic matter which may become slowly available for later
crops. Henzell and Vallis (1977) reported that as much as 30% of the
tropical legume residues were mineralized and taken up by the companion grass
after 24 weeks.
The rate of mineralization of plant materials
also depends on the method of its application.
Fresh plant material mineralizes at a faster rate than dried material
(Schreven, 1968) and buried residues decay at a faster rate than do surface
residues (Moore, 1974).
The mineralization process is affected by
several other factors. Higher soil
temperature enhances mineralization, higher soil moisture reduces
mineralization (Cassman and Munns, 1980).
Cultivation may also enhance the rate of mineralization (Arnott and
Clement, 1966; Powlson, 1980). Addition
of phosphorus in P deficient soils has been found to enhance nitrification
(Purchase, 1974). Grass root extracts have been reported to suppress nitrifying bacteria (Theron, 1951), however, in
lower concentration grass and legume root extracts have also been reported to
increase the rates of N mineralization and nitrification (Odu and Akerle, 1973).
Mineral N from
decomposing plant material may also be lost from the soil in a solution or in a
gas form by leaching, volatilization and denitrification (Tanaka and Mavasero,
1964; Watson and Lapins, 1964; Bartholomew, 1965; Cornforth and Davis, 1968;
Kilmer, 1974).
In an experiment, when
crop residues were plowed under the soil, the N in the returned herbage was
subject to loss unless taken up by plants (Watson and Lapins, 1964). It was reported that when dried clover and
grass herbage (3.86% N) was applied to an annual grass pasture, that for each
100 lbs. of herbage N applied, 11 lbs. were taken up by grass plants, 46 lbs.
were lost by volatilization or leaching, and the remaining 43 lbs. were
recovered in the soil. Other
experiments have also shown the loss of N from plant residues of soybeans
(Suttle et al., 1979), corn (Terman and Allen, 1974) and spring wheat (Boatwrite
and Haas, 1961). Losses of N from urine
(54% N loss) after 8 weeks of urine application in summer (Watson
and Lapins, 1969) and losses of up to 80% of N from cattle dung lying on
the soil surface in a warm climate have been reported (Gillard, 1967). Loss of
nitrates by leaching may be reduced by growing deep-rooted crops like corn, and the role of a deep-rooted crop (like corn) in reducing losses of
nitrate is further enhanced in intercropping systems (Singh et al., 1978).
Significant losses of N are
common from the N-fertilizer applied in to the soil. A review of the literature by Allison (1966) indicated that average crop recovery is about 50% of
the N applied. Other experiments (Soper
et al., 1970; Toews and Soper, 1978) with barley have shown similar recovery
(50%) from N fertilizers broadcasted. N
recovery, however, was increased to 60% by band application of N fertilizers.
The amount of N contribution from legume to
an associated non-legume or to a subsequent crop depends on the N fixing ability
and N requirement of the legume. The
amount of N fixed is determined by many factors including plant species, plant
density, climatic conditions effectiveness of bacterial strain, soil ph and
nutrient status, and the amount of available N in soil (Allison, 1965).
The quantity of N fixed by legumes is
variable and a wide range in amount of N fixed by legumes has been reported
from a few kilograms to 700 kg N ha-1 yr-1 (Nutman, 1971;
Date, 1973; Jones, 1974; Graham and Hubbell, 1975). Annual legumes seem to fix appreciably less N ha-1 yr-1
than perennial legumes due to a shorter growing season for annuals (Nutman,
1971) . In perennials at least one
third of the fixed N is concentrated in the root mass, while in annual legumes,
when ripe for harvesting, most of the N assimilated from the atmosphere is in
the tops of the plants (Sundara Rao, 1975).
A wide range of amounts of N fixed by
mungbeans has been reported by several workers, 6 to 32 kg N ha-1 yr-1
(Gomez and Zandstra, 1976) and 325 kg N ha-l yr-1
(Agboola and Fayemi, l972). Many
workers (Agboola and Fayemi, 1972; Misra and Misra, 1975; Saraf and De, 1975;
Singh and Singh, 1975) demonstrated that mungbeans were more beneficial in rotation with cereal crops than as a companion
crop. Residual N from mungbeans were
reported to be 22 kg N ha-1 (Agboola and Fayemi, 1972) and 25 kg ha-1
(IARI, 1976) in one season. Agboola and
Fayemi (1972) reported an excretion of 3% N fixed by mungbeans at flowering
time.
Various estimates of
amounts of N fixed by soybeans have been reported. In
several experiments, soybeans fixed 84 kg N ha-1 (Weber, 1966a,
1966b), 93 to 160 kg N ha-1 (Vest, 1971), 148 to 163 kg N ha-1
(Weber et al., 1971), and 17 to 369 kg N ha-1 (Gomez and Zandstra,
1976). Schroder and Hinson (1974)
studied the nodulating and nonnodulating soybeans grown in rotation with
winter rye and in mixture with rye, and reported that roots of modulating
soybeans left a considerable amount of N in the soil. Saxena and Tilak (1975) reported that wheat following a soybean crop
received 30 kg N ha-1 as a residual N from the soybean crop.
Perez-Escolar et
al.(1978), using soybean, mungbean and wingbean legumes followed by corn crop,
reported that in all cases corn following the legume had higher yields than corn
following corn. About 80% of the maximum corn yield was attained when corn
followed the legumes and with no fertilizer N applied. Shrader et al. (1966) showed that
approximately 90 kg N ha-1 was available to corn following soybeans.
Leucaena (Leucaena
leucocephala) has been reported to fix a very high amount of atmospheric
nitrogen. The amount of N fixed was
reported as 500 kg N ha-1 yr-1 (Guevarra, 1976) and a
range of 310 to 800 kg N ha-1 yr-1
(Brewbaker et al., 1972; Gomez and Zandstra, 1976). Guevarra (1976), working
with corn/leucaena intercropping, incorporated leucaena in the soil and
reported that leucaena contributed significantly to reducing the nutritional requirement of the
intercropped corn. Yield of
intercropped corn with leucaena incorporation in the soil was comparable to
yield of corn where 75 kg N was applied as urea. Harvesting and
incorporation of leucaena in intercropped corn at early stage of corn was more
beneficial than at later stages.
Sears (1953) reviewed a
number of New Zealand experiments and concluded that 50 lbs. out of 230 lbs. N
A-1 fixed annually by white clover was transferred to associated
grass at one location, and 140 lbs. out of 500 lbs. N A-1 yr-1 was
transferred at another location. Herriott and Wells (1960) found that white
clover transferred about 50% of its fixed N to rye grass and about 33% to orchard
grass. In other cases, however, only a
small amount or no N transfer from legume to associated grasses have been
reported (Walker et al., 1956).
Whitney et al. (1967)
reported that Desmodium intortum fixed 340 lbs. N ha-1 yr-1
and about 5% was transferred to the associated grasses. Transfer of fixed N
from desmodium to the associated grass was reported to be as little as 1.66% in
sand culture (Henzell, 1962) to as much as 20% to pangolagrass (Whitney and
Green, 1969). In small plots (nongrazed)
transfer of nitrogen is small but in grazed plots (through animal urine, trampling, etc.)
transfer would be expected to be much greater (Henzell and Vallis, 1977). Henzell et al. (1966) reported the
accumulation of 90 to 100
lbs. of N A-1 yr-1 in soil by desmodium.
One of the problems
usually observed in cereal/legume intercropping is shading of legumes by
cereals. Shading decreases the
availability of light to the
legume and thus less photosynthates are available for the rhizobium to continue N fixation
(Bethlenfalvay and Phillips, 1977; Eriksen and Whitney, 1982). Reduced nodulation and reduced nitrogen
fixation in legume in cereal/legume intercropping has also been reported in
soybean (Reddy and Chatterjee, 1973; Wahua and Miller, 1978a, 1978b), dry beans
(Graham and Rosas, 1978) and desmodium (Whiteman, 1970).
Kitamura et al. (1981)
studied the competition between Desmodium intortum and Setaria
anceps and reported that nodule numbers were depressed by both top and
root competition but the legume plants were able to compensate by increases in
nodule size and increases in acetylene reduction activity per unit of nodule
weight (specific nitrogenase activity).
Increase in nodule
activity in soybean has been observed with up to 18% shading (Trang and
Giddens, 1980) and with 20% shading (Wahua
and Miller, 1978a, 1978b). Shading reduced the number of small-sized
nodules, and increased
the efficiency of bigger-sized nodules in up to 20% shading then nodule
activity rapidly declined with increasing shade.
Studies of ICRISAT (1977) included the efficiency of nitrogen
fixation in pigeon peas when interplanted with sorghum. Pigeon peas had better nodulation when the
roots intermingled with those of intercropped sorghum. Thompson (1977) reported an apparent
increase in nodule number and weight of soybeans growing with corn. He explained that the cereals depleted soil
nitrogen, thus stimulating the nitrogen fixation by legumes.
Green Leaf Manuring
Green manuring has been
in practice from ancient times and at the present is becoming of increasing
importance due to the increasing costs and unavailability of nitrogenous
fertilizers in many parts of the world.
Green manure crops are those crops grown solely to benefit concurrent of
subsequent crops by increasing soil fertility and improving soil physical
properties. Green-leaf manure crops are grown on adjacent sites
and periodic loppings or prunings are used to fertilize another crop. Legumes, having N fixing capacity and high N
content in foliage, can play a vital role as green manure crops.
Much of the experimental
work on green manures has been done with rice.
In a pot study, Mahalingam et al. (1975) found the yield response to green-leaf
manure N equivalent to calcium ammonium nitrate and greater than ammonium
sulfate when N was applied equally for the sources at 67 kg ha-1. Ali and Morachan (1974) reported that IRRI
rice varieties produced 5.3 and 5.9 t ha-1 grain, respectively, for Crotalaria
juncea green-leaf manure (25 t ha-1 and an equal amount of N
(187.5 kg ha-1 as ammonium sulfate, compared to 4.2 t ha-1
grain when the N was supplied as farm yard manure. Patnalik and Rao (1979), reviewing N sources of rice, concluded
that on an equal-N basis, at moderate levels of 20 to 40 kg N ha-1,
green manure was as efficient as inorganic N.
In one experiment in
Peru, Wade and Sanchez (1983) used kudzu (Pueraria phaseoloidy)
and guinea grass (Panicum maximum) as mulches or as incorporated
green manures under three fertilizers treatments. Kudzu
incorporated
at the rate of 8 tons fresh material/ha/crop produced yields which were 90% of
the crops receiving complete inorganic fertilization (120 kg N ha-1). The beneficial effects of incorporating
kudzu as green manure were associated with the amounts of N, P, K, Ca and Mg released from the
decomposing material, and decreased Al saturation. Mulching produced about 75% of the crop yield achieved with
completely fertilized plots.
In corn experiments, Ruiz
and Laird (1961) found that C. juncea green manure provided 84 to
97 kg ha-1 N in the green matter which resulted in a grain yield
greater than the fallowed control by over one ton, and equivalent to inorganic
N at 80 kg ha-1. Stickler et
al. (1959) in Iowa reported a corn response (95% of maximum yield) to 122 kg ha-1
N in green-manured legume tops and roots as compared to from 56 to 112 kg ha-1
inorganic N.
Residual effects of green
manures on corn are generally nonsignificant, but occasional responses are
reported. Eusebio and Umali (1952)
working with pulses, reported that cowpea green manure increased yields of the
second successive corn crop also. In
Indonesia, Van de Goor (1954) reported that C. juncea grown after corn as green manure for rice increased
corn yield in the following cycle.
Rattray and Ellis (1952) found that the second corn crop grown after a
green manure crop produced only one-half the yields of the first crop.
Evans (1981) using C.
juncea as a green-leaf manure in a corn crop reported that green-leaf
manure produced corn yields equivalent to urea at low (under 100 kg ha-1)
N rates and that the residual effects of
green manure to next crop
of corn was less than 50 kg ha-1 N rate of urea application.
Leucaena with a capacity
for fixing high amounts of atmospheric nitrogen (310 to 800 kg N ha-1
yr-1) and its multiple uses (Brewbaker et al., 1972; Gomez and
Zandstra, 1976) has attracted attention of researchers for its use as green-leaf manure because of its
high N content in foliage. Only limited
work has been done on the leucaena as a green-leaf manure.
There are two basic types
of systems involving leucaena use as a fertilizer and soil ammendment. In the first, hedge rows of leucaena are
intercropped with food crops, also called as "alley cropping." In this system leucaena foliage are
periodically pruned and mulched or incorporated into the soil for use by the
companion food crop growing in the same field.
The second involves sole cropping of leucaena for cutting and
transporting to another field. This
"cut and carry" system constitutes an export of nutrients from one
field to another.
Guevarra (1976)
intercropped corn with leucaena to compare the yield and N uptake response of
corn to N supplied from leucaena greenleaf manure and from urea. He estimated the N contribution of leucaena
green manure (forage) to the corn on the basis of: 1) the concentration of N in
the corn plant tissue samples, 2) the weight of corn seedlings, and 3) grain
yields. He reported that the yield of
intercropped corn with leucaena incorporation was comparable to yield of corn
where urea was applied at the rate of 75 kg N ha-1. The efficiency of leucaena in
supplying N to corn was about 38% of that of urea.
In studies at the
International Institute of Tropical Agriculture (IITA) in Nigeria, Kang et al.
(1981a) used leucaena prunings as green-leaf manures in pot studies and in
field trials in which crops were
grown between widely
spaced hedges of leucaena in a system they called "alley cropping." They found that incorporation of prunings
produced higher corn N-uptake, ear leaf N
concentration, and grain yields than when
applied as mulch. In the alley cropping
trial, grain yields were significantly increased over the control (no N
applied). Application of l00 kg ha-1
of fertilizer N, 10 t ha-1 of leucaena prunings, or 50 kg ha-1
fertilizer N plus 5 t ha-1 of pruning treatments produced 4.5, 3.7,
and 3.5 t grain ha-1, respectively, in contrast to 2.6 t ha-1
for the no N control. Kang et al. (1981b)
in field studies also reported the suitability of leucaena as a green-leaf
manure in corn/leucaena alley cropping system as a low N-input system.
In four year of study of
corn with leucaena in alley cropping, 5 to 6 annual prunings of leucaena yielded
5 to 8 tons of dry prunings
ha-1 yr-1,
which contained 180 to 250 kg N ha-1 yr-1 (Kang et al.,
1981b).
This annual green-leaf
manure addition sustained corn grain yields at 3.8 tons ha-1 yr-1
with no N fertilizer application while yields declined with no green-leaf
manure.
In the above trial (Kang
et al., 1981b), 5 corn rows per “alley” were harvested separately during two
seasons. In the first season, corn
yields were significantly lower in the rows bordering leucaena badges. In the second season, in which the timing of
leucaena prunings was done so as to minimize shading of the corn, there was no
significant difference between yields from various rows. This indicates that shading is a main factor
of competition between intercropped corn and leucaena and that timing of
leucaena pruning must be done to minimize this shading.
In another experiments
(Mendoza et al., 198l), corn was grown alone or intercropped between hedges of
leucaena 3 m apart and herbage from leucaena was applied as green manure at 9.44
t ha-1. Application of green manure increased
corn fodder yields from 3.59 t in corn alone to 8.24 t dry matter ha-1. In a further trial corn intercropped with
leucaena hedges 3 or 4.5 m apart and with 9.85 and 7.84 t green manure ha-1
yielded 11.02 and 9.94 t fodder ha-1 and 8.99 and 7.58 t marketable
ears ha-1, respectively.
Pure corn stands given 45 to 90 kg N gave 4.59 and 14.44 t fodder ha-1
and 9.07 and 8.11 t marketable ears ha-1, respectively.
At IITA in 1981, Read
(1982) studied several important leucaena green-leaf manure management
alternatives, including; application of fresh vs dried leaves, mulching vs
incorporation of leaves, and split application vs application of complete rates
at planting. Results of the corn in
this trial showed that dry weight gain in corn at 40 days was significantly
higher with fresh-leaf than with dry-deaf application. Incorporation was
significantly better than mulching with fresh but not, with dry leucaena
leaves. He also found that there was,
no difference
in applying
the leucaena at planting and splitting the application with 1/3 at planting and
2/3 four weeks later. Read (1982)
determined the field decomposition rates of leucaena by measuring loss of
organic matter in 2 mm mesh nylon bags.
It was found that the decomposition rate of fresh and dried leucaena
foliage was significantly faster when buried rather than mulching.
In Hawaii, Evensen (1983)
evaluated both mulching and incorporation methods of leucaena application in
corn, where leucaena green leaves were applied at the rates of 57, 114, and 171
kg N ha-1. This study showed
that incorporation of leucaena leaves was superior than the mulching
method. N recovery by corn in this
study were found to be 57.9,
31.7 and 18.4% for urea, leucaena leaves incorporated, and leucaena leaves
mulched, respectively.
The
Use of 15N-Labeled Fertilizers
Tracer techniques based an the use of the
stable isotope 15N are common in nitrogen research. The 15N isotope was discovered by
Naude (1930), and practical methods for its use was reported by Urey et al.
(1937). The first application of l5N
in agronomic research was by Norman and Werkman (1943), who used it to study
the uptake of nitrogen by soybeans.
The use of tracers is based on the fact that 14N
and 15N occur naturally in a almost constant ratio. The ratio of 14N to 15N
in nature is found to be 272:1 (Hauck and Bremner, 1976). Addition of l5N material in a
system causes a change in 14N to l5N ratio in that
system, which gives an idea of the extent to which the tracer has interacted
with and become a part of the system.
At present, the ratio of (14N14N) to (14N15N)
is measured by mass a spectrometer and recently also by an emmision
spectrometer.
Reviewing the literature, Hauck and Bremner
(1976) indicated that nitrogen tracers have been used to study nitrogen
mineralization - immobilization reactions in soil, gains of N by, and losses of
N from soil and water, plant recovery of applied N, N movement through soils to
water, N balance in ecological systems, and virtually all known aspects of N
cycle processes.
Several recent works indicated extensive use
of 15N-tracer technique in many areas of research: N fertilizer
efficiency (Tomar and Soper, 1981; Wetselaar,
1983), N leaching (Malhi and Nyborg, 1983; Priebe et al., 1983; Sompangse et al., 1983),
denitrification (Malhi and Nyborg,
1983; Novak and Blackmer, 1983), decomposition of plant residues (Herridge,
1982), N transfer from legume to grass (Ismaili, 1983) and N excretion by
legumes (Burton et al., 1983).
The use of 15N-tracers
has made it possible to study the proportion of N derived from fertilizers,
soil and atmospheric fixation. In nonleguminous
plants, where the N sources are only soil N and fertilizer N, the proportion of
N derived from the applied fertilizer can easily be measured with the use of 15N-labeled
fertilizer. In case of leguminous
plants, where three sources of N are available for plant’s use, however, this analysis becomes
complex.
The first use of 15N
in N2 fixation research was by Burris and Miller (1941) in
studies of N2 fixation by Azotobacter vinelandii. Since then there has been extensive use of 15N-tracers
for measuring N2 fixation.
Even with the use of 15N-tracer, the problem remains there as
the total N of plants consist of labeled N from fertilizers, and unlabeled N
from soil and fixed N and it is difficult to separate soil N from fixed N,
since both are unlabeled. This problem
was resolved by Fried and Broeshart (1975) who suggested the use of non-fixing
crop as the reference crop adjacent to fixing crop. In this method 15N-labeled fertilizer is applied to
both non-N-fixing and N-fixing crops grown under identical soil
conditions. The available amounts of
soil plus fixed N are determined using the legume crop, and the available amount
of soil N is determined using the reference crop.
Legg and Sloger (1975)
developed a 15N-tracer technique better suited for evaluation of N2
fixation under field conditions in
which they incorporated 15N into the soil organic N, and then this 15N-labeled
soil organic matter was used as the tracer material. The use of 15Nlabeled soil organic matter (Legg and
Sloger, 1975) may have two advantages over the 15N studies
in which 15N-labeled fertilizer is used as the tracer material
(Fried and Broeshart, 1975). The first
advantage is that incorporation of 15N into the soil
organic fraction using carbon substrate also ties up the available soil N,
thus, the N input from the soil results from mineralization of labeled soil organic N,
in contrast to 15N fertilizer methods, where the N inputs
from soil consist of soil and fertilizer N.
The second advantage is that the incorporation process reduces the
amount of combined N available to the plants and thus promotes N2
fixation. The 15N fertilizer
method, in contrast, increases the amount of available N which tends to depress
N2 fixation levels (Harper, 1976).
The use of 15N-tracers for the measurement of N2
fixation has recently become popular (Fried and Broeshart, 1981; Broadbent et
al., 1982; Rennie, 1982; Rennie et al., 1982; Talbott et al., 1982; Wagner and
Zapata, 1982; Jones and Foster, 1983).
15N-tracer techniques have
also been used in studies dealing with evaluation of uptake of N from plant
residues (Yaacob and Blair, 1980; Herridge, 1982). Herridge (1982) grew a wheat crop on soil amended with 15N -labeled plant residues
of Medicago spp. and deported that only 11-17% of the 15N-labeled medicago residues added
to the soil were utilized by a succeeding wheat crop, while 72 to 78% remained
in the soil organic pool.
In another experiment,
Yaacob and Blair (1980) used soil from plots that had grown 1, 3, or 6 crops of
soybeans or siratro. 15N -
labeled residues from soybeans and siratro were added to half the plots in the
experiment and the other half was left unamended, and then rhodegrass was
grown. They reported that N uptake by
the grass increased with number of previous cycles and was higher in siratro than soybean
soils. The total recovery of 15N from
soybean residues were 14.7, 14.6 and 16.8% from soils cropped to 1, 3 and 6
previous soybean crops, respectively.
In contrast,
the total 15N
recovery from siratro residues were 13.7, 42.4 and 55.5% from soils cropped to
1, 3 and 6 siratro crops,
respectively.
In an experiment,
Pomares-Garcia and Pratt (1978) used various rates of manure and sludge
combined with 15N-labeled ammonium sulfate and grew barley and
sudangrass as test crops. He reported
that 37.2 to 70.2% of the N from ammononium sulfate was recovered by the first
cutting of barley forage and a range of 0.7 to 8.9% recovered by sudangrass, which was the last crop
of the cropping sequence.
In a recent study, Ladd
et al., (1983) grew two crops of wheat on a soil mixed with ground 15N-labeled
legume material (Medicago littoralis) and reported that the first
wheat crop took 20.2 to 27.8% of the legume N applied at the rate of 48.4 kg ha-1. The uptake of N from legume residues to a second wheat crop declined to 4.8% of
legume N applied. For both first and
second wheat crops, uptake of N from legume residues was approximately
proportional to legume N input over the range of 24.4 to 96.8 kg ha-1. The proportions of wheat N derived from
added legume N were 32 to 65% for grain and 5 to 6% for roots. These studies
indicate that 15N-labeled organic residues can successfully be used
in the evaluation of N uptake
from plant residues.
Evaluation of Intercropping
Experiments
The evaluation of
cropping system in intercropping situation become more complex as compared to
monocropping situations, where only one crop is involved. When two crops are grown in intercropping,
one crop interferes with another, and therefore, they cannot be considered
growing independently, hence yield performances cannot he evaluated separately
in intercropping experiments.
To fully analyze the
intercropping situation, one needs to combine the performances of all crops in
some way, however, and this is where difficulties arise. Strict addition of yields is usually
meaningless where they are of very different types, but this is usually the
case in most intercropping experiments.
It was suggested that the yield performances in intercropping
experiments be converted in terms of some common parameters (Willey, 1979b).
Usually two approaches
are used to evaluate intercropping experiments. One is an economic approach, where crop yields are converted in
terms of money, and then cost/benefit, profitability or monetary advantages are
calculated. The other is an energetic
approach, where crop yields are converted in terms of calories, proteins,
nitrogen, digestible nutrients, dry matter etc. to evaluate the total
productivity in the intercropping situation.
These conversions to common parameters provide opportunity to better
evaluate the intercropping situation even with crops of diverse nature. Objections were raised however by Pearce and Gilliver
(1978) in using these two approaches for evaluation, who said that the monetary
value is subject to fluctuating market conditions. Caloric value may appeal to the dietician but it does not enter into the
consciousness of the peasant farmer, who is the one to be persuaded.
The main objective of
most intercropping experiments has been to investigate the output of the
intercrop compared with the monocrop situation and to whether or not
intercropping provides any advantage over monocropping. The most commonly used method of evaluating
intercropping experiments is the use of the Land Equivalent Ratio (LER). LER is defined as the relative land area under
monocrops that is required to produce the yields achieved in intercropping
under the same
management
(Willey, 1979a). LER is calculated as
the sum of the ratios of dry weight yields of each crop in a mixture over its
yields in pure culture. LER provides an
accurate assessment of competitive relationships between components as well as
overall productivity of the intercrop system.
When, LER = 1 , the overall yield per unit of area of intercrop is never
greater than that of the
most productive monocrops, and there is no yield advantage in intercropping. In another situation, if LER > 1, it
implies that the intercrop outyields the monocrop and there are yield
advantages in intercrop over monocrop.
Another method used in
competition studies is the
Relative Yield Total (RYT) by de Wit and Van den Bergh (1965). RYT is calculated in the same
way as LER, but it is on a yield basis rather than a land-area basis as in
LER. A mixture of crops could be
economically advantageous if the RYT is greater than 100%.
In addition to LER and
RYT, methods such as calculations of Relative Crowding Coefficient,
Aggressivity and Competition Index are used to describe competitive
relationships and to evaluate yield advantages in intercropping experiments
(Willey, 1979a). Relative Crowding
Coefficient was proposed by de Wit (1960) and examined in detail by Hall
(1974a, 1974b). In this method, each
species has its own coefficients (K) which gives a measure of whether the
species has produced more, or less yield than expected. Relative Crowding Coefficient is calculated
as the ratio of yield of a species in mixture over the yield difference between
yield in pure stand and yield in mixture.
If the product of Relative Crowding Coefficient of all species, K >
l, then there is yield advantage, if K = 1 there is no differences, and K <
l then there is yield disadvantage.
Aggressivity, proposed by
McGilchrist (1965), gives a simple measure of how much the relative yield
increase in species "a" is greater than that for species
"b". In a mixture
of two species, Aggressivity can be calculated as the difference between the
ratio of mixture yield of "a" over expected yield of "a" to
mixture "b" over expected yield of "b". An Aggressivity value of zero indicates that
the component species are equally competitive.
For dominant species this value is positive and for dominate species the
value is negative.
A Competition Index was
suggested by Donald (1963). The basic
process is the calculation of equivalence factors for each species. For species "a" the equivalence factor
is the number of plants of species
"a" which is
equally competitive to one plant of species "b". If a given species has an equivalence factor
of less than one it means it is more competitive than the other species. The competition index is the product of the
two equivalence factors. If the
competition index is less than one there has been an advantage of mixing
species.
In terms of economic
approach of evaluation, monetary advantage is quite often calculated, where
monetary advantage = value combined intercrop yield X (LER - 1)/LER. Income Equivalent Ratios are sometimes used
(conversion of LER into income terms).
It is the land area needed under sole cropping to produce the same gross
income as in one hectare of intercropping at the same management level. However, Land Equivalent Ratio and Relative
Yield Total are most commonly used to evaluate intercropping experiments.
CHAPTER III
GRAIN LEGUMES WITH OR
WITHOUT INTERCROPPING
WITH CORN (Zea
mays L.)
INTRODUCTION
Legumes are frequently
grown with cereals in multiple cropping systems to increase food production
per hectare of land. In addition to
increased productivity per hectare of land, the practice of intercropping a
cereal and legume is based on the hypothesis that the cereal can utilize nitrogen
fixed by the legume. Legumes may
contribute N to associated cereals or to succeeding cereal crops.
In general, yield advantages are observed in intercropping over monocropping. Among the
several crops used in intercropping, corn is one of the major cereal crops
widely used in cereal/legume intercroppings. Among the several grain legumes intercropped with corn,
mungbean is becoming popular as it matures in a short period of time and thrives under a wide range of conditions (Ahmed,
1976). Yields of corn in corn/mungbean intercrops were significantly
higher than the yields of corn as monocrops in several studies (Agbboola and
Fayemi, 1972; Gunasena et al., 1979; Das and
Mathur, 1980; Rathore et al., 1980). Other studies of corn/mungbean intercropping indicated that corn yields were not
affected but the yields of mungbeans were depressed (Agboola and Fayemi,
1971; Ahmed, 1976; Singh and Chand, 1980).
Soybeans are also widely used in intercropping
with corn (Chatterjee and Roquib,
1975; Nair et al., 1979). A wide range of results have been reported
in corn/soybean intercropping experiments.
Some experiments showed increase in corn yields when intercropped
with soybeans over monocrops (Narang et al., 1969; Jagannathan et al., 1979;
Kalra and Gangwar, 1980; Singh et al., 1980; Srivastava et al., 1980). Other experiments showed a decrease in corn
yields when intercropped with soybeans over monocrops (Wong and Kalpage, 1976;
Dalal, 1977; Cordero, 1978). Most studies
involving corn/soybean intercropping, however, indicated that corn yields were
usually not affected but the soybean yields were depressed (Roquib et al.,
1973; Singh, 1977; Mohta and De, 1980; Chowdhury, 1981; Searle et al., 1981).
The N contribution from
legume to an
associated or to a succeeding crop basically depends on the N fixing ability and N requirement of the legume. The quantities of N fixed by legumes vary
widely from a few kilograms to over 700 kg N ha-1 yr-1 (Date, 1973; Jones, 1974; Graham and Hubbell,
1975).
The amount of N fixed by mungbeans has been reported to vary
from 6 to 32 kg N ha-1 yr-1 (Gomez and Zandstra, 1976) to as much as 325 kg N
ha-1 yr-1
(Agboola and Fayemi, 1972). Many
researchers have demonstrated that mungbeans were more beneficial in rotation
with cereal crops than as the companion crop (Agboola and Fayemi, 1972; Mora
and Misra, 1975; Saraf and De, 1975; Singh and Singh, 1975; IARI, 1976).
Estimates of amount at N
fixed by soybeans vary widely from 17 to 369 kg N ha-1 (Weber,
1966a, 1966b; Vast, 1971; Weber et al., 1971; Gomez and Zandstra, 1976). Residual N from soybeans supplied to a following crop has varied from 30 to 90
kg ha-1 (Shrader et al., 1966; Saxena and Tilak, 1975).
The N contribution from legumes to associated
non-legumes or to succeeding crops may be different, since legumes differ in
their abilities to fix atmospheric N2. The N economy may also differ due to different growth habits of
legumes. No work has been reported
which examines the N contribution from determinate and indeterminate types of
the same grain legume species.
Therefore, there is need to investigate the N contribution from such
legume types to an associated cereal crop.
Research on cereal/legume intercropping has
been done at different locations under very different environmental conditions. Considerable
variability among sites occurs due to differences in initial soil
fertility and/or other environmental factors.
To avoid the confounding effect of these site specific variations and to
provide more precise comparisons of legumes in cropping systems, it becomes
important that legumes be intercropped with cereal at one location in over
several crop cycles.
The experiment reported here was conducted to evaluate the yield potentiality
and N economy of intercropping two grain legume species with corn.
MATERIALS AND METHODS
A field experiment involving intercropping of
two annual grain legumes (mungbeans and soybeans) with a main, crop of corn was
conducted during four consecutive growing seasons beginning June 15, 1981 at
Waimanalo Research Station located at an elevation of 20 meters and at a
latitude of 21oN. The soil
at this site is class tied as the very fine kaolinitic, isohyperthermic family of Vertic
Haplustolls and belongs to the Waialua
series.
Removal of Available
N from Soil
Two crops of sweet corn
were grown in
the field to
reduce the amount of available N
from the soil
before starting the experiment. The first and the second crop
of sweet corn were planted an October 8, 1980 and January 30, 1980 respectively in order to insure the
proper growth of sweet corn, P and K were applied at the rates of 100 and 90 kg ha-1,
respectively. The second sweet corn
crop showed sever N deficiency, and as a consequence very poor growth was
observed. N content in ear leaves of the
first and the second crop of sweet
corn at the 50% silking stage were 2.70 and 1.22%, respectively. The second crop of sweet corn was harvested on May 15, 1981.
Fertilization
After plowing and tilling of soil, P as
triple super phosphate
and K as
muriate of potash
were applied
at the rates of 120 and 100 kg ha-1, respectivley, for
all crops in each season. N was applied
as urea at four levels ( 0, 33, 67, 100 kg N ha-1) only
for the corn monocrop in each
season. Treatments loving legume monocrops and legume
intercrops with corn were not supplied with N.
Planting of the Experiment
Corn variety H 763 was grown us the main
crop. Mungbeans (Vigna radiata) var. VC
1974A (determinate) and var. V 2013 (indeterminate), and soybeans (Glycine
max (L.) Merr.) var. Davis were the grain legumes used in this experiment.
Legume seeds were
inoculated with effective strains of Rhizobium before
planting.
Mungbean seeds were inoculated with a mixture of TAL 169, TAL 420 and
TAL 441 strains of Rhizobium sp., and soybean seeds were
inoculates with a mixture of TAL 102,
TAL 377 and TAL 379 strains of Rhizobium
japonicum.
The experiment was
arranged in
a randomized
complete block design with 4 replications and 10 treatments. The sequence of crop combinations and crop rotation used are given
in Table 3.1. Monocrops of corn were
grown at four levels of N (0, 33, 67, and 100 kg ha-1) and were
continued from seasons 1 to 4 by adding the same given rates of N in each season (treatments 1 to 4). Mungbeans (both determinate and indeterminate) and soybeans were grown with
or without corn (treatments 5 to 8) in seasons 1 and 3, and those grain legume plots were followed by a monocrop of corn in
season 2 and
season 4.
Spacing and plant density
of crops grown in this experiment are presented in Table 3.2. Mungbeans and soybeans were planted at densities of 606,061 and 400,000
plants ha-1, respectively, in both monocrops and intercrops. Monocrops and intercrops of corn were planted at the densities of 53,333 and 40,000 plants ha-1,
respectively. Corn rows in intercrops
had wider spacing than that
of monocrops. Row spacing in soybeans
was 50 cms in season 1, but was changed to 33 cms in season 3, maintaining the
same plant density. Planting patterns are shown in Appendix
figure 1. Planting dates are presented in Table
3.2.
Weed
and Insect Control
In the plots where only corn was planted,
both Atrazine and Lasso preemergence herbicides were applied at the rate at 2
kg ha-1 of each. However, in the plots where legumes were grown,
only Lasso was applied at the rate of 2 kg ha-1. Weeds were also controlled by hand weeding
whenever necessary.
Diazinon and Sevin (at the rate of 12 ozs
each in 100 gallons of water) were used to control insects (mainly Rose beetle) whenever needed.
Harvesting
Corn and all grain legumes were harvested
whenever they matured. Harvesting dates
are presented in Table 3.2. Sampling
areas at the time of harvesting in corn monocrops and intercrops were 6.75 and
6.00 m2, respectively
(Appendix Figure 1). A sampling area of 6 m2
was used for
mungbeans and soybeans in both monocrop and
intercrop cultures.
|
|
Plant Height, Number of Pods Per Plant
and LAI
Plant heights of 10 plants from each
treatment were measured at time of flowering in each crop and mean values were
used for plant heights.
Pods from each of 10 plants from mungbeans
and from soybeans were counted at maturity and mean values were used as the
number of pods/plants for these two crops.
Leaves from 5 plants in each of the
treatments in corn, mungbeans and soybeans were taken and then leaf areas were
measured with a Leaf Area Meter (LICOR
-CI-3100). Leaf Area Indices (LAI calculated
as leaf area per unit of land) were measured
only in season 1.
Nitrogen Fixation
N2 fixation by
legumes was estimated by the Acetylene reduction technique (Hardy et al.,
1968). Four plants were dug at the time
of flowering from each of the treatments and ethylene produced/plant/hour
(total nitrogenase activity, TNA) and ethylene produced/gram of nodules/hour
(specific nitrogenase activity, SNA) were calculated. Number of nodules/plant
and nodule mass/plant were also recorded.
The ratios of ethylene produced/plant/hour by monocrop Of
legumes to intercrop of legumes were
also calculated.
Dry Matter Yield
Grain yields and stover
(above ground material excluding grain) yields were measured in corn, mungbeans and
soybeans. Total dry matter production
was calculated by the addition of all components. Yields are reported in Megagrams per hectare (Mg ha-1),
which is a metric ton or million grams per hectare.
Nitrogen Content
Ear leaf samples from
corn plants were taken at the 50% silking stage in each season, and then were
analyzed for N content. Grain, stover,
root and nodule samples were also taken after each harvest and then were analyzed
for N content by the Microkjeldahl method (Bremner, 1965a), and total N
production was calculated.
Soil samples from
individual plots were taken before and after each crop season, and were
analyzed for available NH4-N and NO3-N by the steam distillation method
(Bremner, 1965b).
Nitrogen Recovery
Nitrogen recoveries from the
applied urea fertilizer
were calculated in all seasons. N recovered was calculated
as:
N uptake by plants N uptake by plants
with N added -
with no N added
% N recovery =
---------------------------------------- X 100
Rate of N applied
Evaluation
Productivity per hectare
of land was estimated by calculating land equivalent ratios (LER) for all
intercroppings plots. The calculation was done as:
Corn intercrop yield Legume Intercrop yield
LER =
-------------------- + -----------------------
Corn monocrop yield Legume monocrop yield
A harvest index (HI) was
calculated for each crop as: HI = economic yield/ biological yield, where grain yield was the
economic yield and above ground total dry matter was used as the biological yield.
Nitrogen contributions
from legumes to their associated corn crops were estimated by comparing the N uptake by
corn in intercropping with the N uptake by corn in monocropping at 4 levels of N
application. Nitrogen contributions to the succeeding crop of
corn were also estimated by the same approach.
Data were analyzed by an
analysis of variance technique. F
tests, Duncan’s multiple range tests, simple correlation techniques and
regression analyses also were used wherever applicable.
RESULTS
AND DISCUSSION
Performance of Corn in
Intercropping
Grain yield of corn grown
as a monocrop increased dramatically with increasing rates of applied N (Figure
3.1). Grain yields varied from 0.39 to
4.28 Mg ha-1 in season 1 and from 0.55 to 4.82 Mg ha-1 in season 3 as
N rates were increased from 0 to 100 kg ha-1. Figure 3.1 shows very good linear response
of N application by corn with a reasonably high R2 of 0.88 in both
seasons 1 and 3. The slopes of the
regression lines show that with every kg of N applied, grain yields of coal
increased by about 37 kg in season 1 and 43 kg in season 3. Low yields without applied N (control plots)
were probably due to the removal of available soil N by two crops of sweet corn
grown previously which also may account for the good response of corn to N.
Corn grain yields in
intercroppings were higher than the grain yields in control plots (no N
application) in both seasons 1 and 3 (Figure 3.2 and Appendix Table 1). Compared to grain yields of corn in control
plots in season 1 (0.39 Mg ha-1) and season 2 (0.55 Mg ha-1),
the grain yields in intercrops were 0.61, 0.63 and 0.63 Mg ha-1 in
season 1, and 1.00, 0.80 and 0.65 Mg ha-1 in season 3 in
corn/determinate mungbeans (MBD), corn/indeterminate mungbeans (MBI) and
corn/soybeans, respectively. The
increase in corn grain yields were 158, 168 and 163%
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over the control in
season 1, and 181, 146 and 118% over the control in season 3 in corn/MBD,
corn/MBI and
corn/soybean
intercroppings, respectively (Table 3.3).
The results showed that corn when intercropped with mungbeans or
soybeans did not suffer competition from legumes, instead had yield advantages
in the companionship of grain legumes grown in this investigation.
These results agree with
other findings where increase in corn yields were found when intercropped with
mungbeans (Agboola and Fayemi, 1972; Gunasena et al., 1979; Das and Mathur,
1980; Rathore et al., 1980) and with soybeans (Narang et al., 1969; Nair et
al., 1979; Kalra and Gangwar, 1980; Singh et al., 1980; Shrivastava et al.,
1980).
Total dry matter of corn
in monocrops increased with increasing rates of N application (Figure
3.2). The increase in total dry matter
yields were from 3.08 to 10.01 Mg ha-1 in season 1 and from 4.33 to
13.36 Mg ha-1 in season 3 at N rates of 0 and 100 kg ha-1,
respectively. The total dry matter
yields of corn in intercrops, however, were not different from those in the
control plots in both seasons 1 and 3 (Appendix Table 1).
Harvest indices (HI) of
corn increased from 0.12 to 0.43 in season 1 and from 0.13 to 0.36 in season 3
as N rates increased from 0 to 100 kg ha-1 (Table 3.4). HI of corn
when intercropped increased slightly (a range of 0.20 to 0.24 in season 1 and a range of 0.15 to
0.19 in season 3), but not significantly compared to the control plots of corn
(0.12 and 0.13 in seasons 1 and 3, respectively). This slight increase in HI in intercrops was not unexpected as
there was an increase in grain yields, but no change in total dry matter of
corn in intercrops.
Plant height of corn
increased with increasing rates of N application in both seasons 1 and 3
(Figure 3.3). There was a slight but
non-significant increase in plant height of intercropped corn compared to
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the monocropped corn
(control plot) in season 1. In season
3, there was a significant increase in plant height of intercropped corn
compared to the control plot of corn. In season 3, plant heights
of corn were 1635, 1656 and 1613 mm in corn/MBD, corn/MBI and corn/soybean intercroppings, respectively, compared
to 1376 mm in the control
plot of corn. These results also
indicate that
corn grown with mungbeans or soybean did not suffer from competition with legumes.
Performance of Grain
Legumes in Intercropping
Grain and total dry
matter yields of mungbeans and soybeans were depressed when grown as intercrops compared to their monocrops in both seasons
1 and 3 (Figure 3.4 and Appendix Table 1).
Except for the grain yields and total dry matter of indeterminate
mungbeans in season 3, the reduction in grain yields and total dry matter in
all other treatments of mungbeans were significant. Soybean grain yield was not significantly reduced when
intercropped in season 3, but was significantly reduced in season 1. This may have been due to greater shading of soybean by corn in season 1 than in season 3, as the distance between corn rows and
soybean rows was 25 cm in season 1 and 33 cm in season 3 (Table 3.2 and
Appendix Figure 2).
Plant heights, number of
pods/plant and harvest indices of mungbeans and soybeans are presented in Table 3.5. Plant heights and number of pods/plant of
intercropped mungbeans generally were not significantly affected by
intercropping. However, the height and
number of pods/plant of soybeans were significantly reduced by intercropping in
season 1, where soybean was shaded by corn.
There were no significant changes in harvest indices of mungbean and
soybean in intercrops compared to monocrops in both seasons 1 and 3. Among the
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two types of mungbeans
used in this experiment, indeterminate mungbeans had a greater number of
pods/plant and was taller than determinate mungbeans in both season l and
season 3. The grain yields of
indeterminate mungbeans, however, were not significantly different than the
grain yields of determinate mungbeans (Figure 3.4).
As previously discussed
in this chapter, there were yield advantages for corn intercropped with grain
legumes, but the above results indicate that there were yield depressions in
grain legumes intercropped with corn.
Therefore, in these corn/grain legume intercrops, corn was dominant over
grain legumes (see also in Appendix Figure 2 and Appendix Figure 3).
These results agree with
those of similar experiments where yield reductions with intercropping were
observed in mungbeans (Agboola and Fayemi, 1971; Ahmed, 1976; Singh and Chand, 1980) and in soybeans (Roquib et
al., 1973; Singh, 1977; Mohta and De, 1980; Chowdhury, 1981) grown with corn.
Total Performance in
Intercropping
Total dry matter yields
of crops in intercropping systems compared to monocropping systems in seasons 1
and 3 are presented in Figure 3.5. In season 1, intercrops of corn/grain legume
produced as much total biomass as legume monocrops. The total biomass produced by these intercrops was comparable to
the total biomass produced by a monocrop
of corn (10.01 Mg ha-1) with 100 kg ha-1 of
applied N. In season 3, total biomass produced by corn/legume intercrops was
higher than biomass produced by legume monocrops, and was comparable to the
total biomass produced by the corn monocrop (10.08 Mg ha-1 ) with
67 kg ha-1 of applied N. The
total biomass produced by corn/legume
intercrops was 3.03 to 5.70 Mg ha-1 higher than biomass produced by
the control plot (3.08 Mg ha-1) in season 1, and 5.37 to
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6.55 Mg ha-1 higher than the biomass produced by the control plot
(4.33 Mg
ha-1) in season 3
(Appendix Table 3). These results
suggest that much higher total can be produced by corn /legume intercrops then by a corn monocrop
application.
Total grain production in monocropped
(control plots) and in intercropped
treatments is shown in Table 3.5. Grain yields of intercropped corn in
both seasons 1 and 3 were higher than those of monocropped corn without N. Moreover, the grain yields of legumes were
additional yields produced in intercrops which would not have obtained
in monocrops of corn without applied N.
The intercropping systems used in
this investigation produced total
grain yields (corn + grain legumes) in the range of 1.58 to 2.05 Mg ha-1
in season 1 and 2.10 to 3.45 Mg ha-1
in season 3 compared to control plot (monocropped corn without N) yields
of 0.39 Mg ha-1 in season 1 and
0.55 Mg ha-1 in season
3. The total grain produced in
intercropping was much higher (about 4 to 5 times in season 1 and 4 to 6 times in season 3) than grain produced by control plots of corn. This suggests that in the areas where N fertilizers are not
easily available or are expensive and food production is the prime objective
one can still obtain substantially higher food production/ha by corn/legume
intercropping than by monocropping corn with no N application.
Leaf areas per unit area
of Land (LAI)
of corn in
intercrops were comparable to the LAI of monocrop of corn (1.64) at 33 kg N ha-1
in season 1 (Table 3.7). LAI’s of
legume intercrops were lower than LAI’s of legume monocrps. Total LAI’s in intercrops (3.25 to 3.80)
were slightly higher than
those in legume monocrops (2.84 to
3.29). Total LAI in corn/legume
intercrops (3.25 to 3.80) were higher than the LAI of the corn monocrop (2.74)
with 100 kg
ha-1 of applied N.
As the LAI of
intercropped corn was as much as or higher than the LAI of the control plot of
corn, these LAI values suggest that corn
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did not suffer from
competition with legumes. The LAI’s of intercropped legumes were lower than
LAI’s of legume monocrops, which
suggests that grain legumes were dominated by corn. This may be the reason for depressed yields of intercropped
legume. The higher total LAI in
corn/legume intercrops indicate
a greater interception of incoming solar radiation by intercrops than by
monocrops, and this may also he the reason for increased total biomass
production/ha in intercropping systems.
Land equivalent ratios
(LER) of corn/grain legume intercrops are presented in Table 3.8. LER of intercropped corn were 1.5 in season 1 and ranged from 0.8 to
1.1 in season 3. Values of LER greater
than one indicated that there were yield advantages of corn when intercropped
with grain legumes. LER of grain legumes were in the range of 0.4 to 0.7 in
season 1 and 0.6 to 0.9 in season 3.
LER values less than one indicate that the yield of grain legumes were depressed in intercrops. The total values
of LER were in the range of 1.9 to 2.2 in season 1 and 1.6 to 1.9 in season
3. These high values of LER indicate
chat one would have needed 1.9 to 2.2 hectares of land in season 1 and 1.6 to
1.9 hectares of land in season 3 under monocrops to produce as much as were
produced in one hectare of land by these intercrops.
The higher LER values
clearly suggest that there were yield advantages in corn/legume intercrops over
corn monocrops with no
N applied. In those areas where N
fertilizers are in short supply and/or are too expensive for a former to use, the use of
corn/legume intercropping systems seems a cheap methods of increasing food
production/ha without input of inorganic N.
Corn Following Grain
Legumes
Grain and total dry matter yields of corn following grain
legumes
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in season 2 and season 4
are presented in Table 3.9. The grain yields of corn in both season 2
and season 4 were poor. In season 2,
the highest corn grain yield (0.57 Mg ha-1) was at the 100 kg ha-1
level of applied N and it was significantly higher than the yields of all other
treatments which were not
significantly different from each other.
Total dry matter yields in season 2 also did not differ in all the
treatments except for those of the 0 and 33 kg ha-1 rates of N which
were significantly lower than those of the other treatments.
In season 4, grain yields
of corn following the indeterminate
and soybean monocrops
were comparable with corn at the
67 and 100 kg ha-1 levels of N.
Grain yields of all other
treatments were comparable to that of at 33 kg ha-1 level of N
application. Total dry matter yields of
corn following monocrops of indeterminate mungbeans
and soybean were comparable to 67 kg ha-1 level of N in the
corn monocrop, and total dry matter yields in all other treatments were
comparable with that of the 33 kg ha-1 level of N. Corn yields in
season 4 were a little better than yields on season 2.
Nitrogen response by corn monocrops was also
found to be poor in Figure (3.6). Grain
yields of corn increased from 0.38 to 0.57 Mg ha-1 in season 2 and
from 0.39 to 0.99 Mg ha-1 in season 4 as N rates were increased from
0 to 100 kg ha-1. Figure
3.6 shows that the response to
N application by corn was linear, but with a poor R2 of 0.35 in season 2 and a little batter R2
of 0.77 in season 4. Slopes of the regression lines show that with each kg of N
applied, the increases in corn grain yields were only about 2 kg in season 2 and 6 kg in season 4. These results show that the N response by corn in seasons 2 and 4 was
much poorer than those of in seasons
1 and 3 (Figure 3.1 ).
There was no significant difference in harvest indices
(HI) in all the treatments in seasons 2 and 4 (Table 3.10). Harvest indices were in the narrow range of
0.15 to 0.21 in season 2 and 0.20 to 0.25 in season 4. These
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results were obvious because grain and total
dry matter yields themselves were not significantly
different among most of the treatments in season 2 and season 4.
Plant heights of corn in all plats having
grown grain legumes in the previous season were comparable to the plant height of monocropped corn with 67 kg
ha-1 level of N application in season
2, and plant heights of the 33 and 67
kg N ha-1 treatments in season 4 (Table 3.10).
The poor performance of
corn in seasons 2 and 4 were due to the fact that these seasons were in the
winter period with lower solar radiation and lower temperature,
which were not favorable for the growth of corn (Appendix Table 3). Also storm with heavy rainfall occurred in
January 1982 during season 2. This
combination of all these environmental factors resulted in poor growth
of corn. Poor growth and thereby poor
yield of corn during the winter was also reported by Jong et al. (1982) in an
experiment where 41 successive monthly
plantings of corn was done at Waimanalo Research Station in
Hawaii.
Environmental Effects
Seasonal yields of corn
were affected by conditions (Figure 3.7).
Corn grain yields in summer plantings of season 1 (0.39 to 4.28 Mg ha-1)
and season 3 (0.55 to 4.28 Mg ha-1)
were much higher than the yields in winter
plantings of season 2 (0.38 to 0.57 Mg
ha-1) and season 4 (0.39 to 1.0 Mg ha-1). The pattern of seasonal yields of corn
followed the pattern of solar radiation.
Average monthly solar radiation in MJ m-2 day-1
during the summer ranged from 6.70 to 22.10 in season 1 and 6.39 to 16.63 in season
3, and during the winter ranged from 6.30 to 10.96 in season 2 and 7.01 to
14.08 in season 4. Average monthly
solar radiation (MJ m-2 day-1) for each of these
seasons was in the decreasing order: 18.20 > 13.50 > 10.18 > 8.18 for
seasons 1, 3, 4, and 2, respectively.
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Grain yields of corn
followed similar trends at four levels of applied N with increasing amounts of
solar radiation, however, N response was poor in the winter (seasons 2 and 4) and was
lowest in season 2. This poor response
to N in season 2 could have been due to the low average solar radiation, and the very high rainfall during that season (Figure 3.7). Average monthly rainfall during the experimental period were 53, 239, 102, and 121 mm in seasons l to 4, respectively. The high average
monthly rainfall (239 mm) during season 2 probably caused leaching of N into
the soil and, therefore, little N was available to the growing plants.
It can be seen that lower
solar radiation associated with higher rainfall (Figure 3.7). The correlation coefficient (r) between
solar radiation and rainfall was -0.88 during the entire period of this
experiment.
The average monthly temperatures (0C)
during these seasons
were 25.1, 22.5, 24.6, and 23.7
in seasons 1 to 4, respectively, with higher
temperature occurring in summer and lower temperatures in winter.
However, the change in
temperature during the entire period of the experiment was gradual and not as
drastic as that observed in solar radiation and rainfall. The
correlation coefficients (r) for the relationships between temperature and solar
radiation, and between temperature and rainfall
during the entire period of the
experiment were 0.94 and -0.97, respectively.
These results clearly show that the corn yields were greatly affected by
changes in environmental conditions during
the growing period of corn.
Nitrogen Yield and Transfer
Nitrogen yields in
monocrops and in intercrops in both season 1 and season 3 are presented in Figure 3.8. N yields of corn in intercrops (18.4 to 19.9
kg ha-1) were not significantly different from the N yield of corn
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in the control plot (18.6
kg ha-1) in season
1; however, in season 3, N yields of corn in intercrops (25.2 to 33.5 kg ha-1)
were comparable to the N yield of monocropped corn with 33
kg N ha-1 (32.64 kg ha-1). These results suggest that there was no N
transfer from grain legumes to corn while they were growing together in season
1, but there may have been some N transfer in season 3. These results also suggest that legumes
did not compete with corn for soil N in the intercropping situation.
Nitrogen yields of grain
legumes in intercrops were lower than the N yields in monocrops in both seasons
1 and 3 (Figure 3.8). Soybeans had much
higher N yields (115 to 234 kg ha-1 in season 1 and 290 to 334 kg ha-1 in season 3)
than mungbeans (110 to 166 kg ha-1 in season 1 and 96 to 154 kg ha-1
in season 3). Nitrogen yields in
determinate mungbeans were not different from N yields in indeterminate
mungbeans in both seasons 1 and 3. The
decrease in N yields of grain legumes in intercrops compared to monocrops may he due to the fact
that legume yields were depressed in intercrops compared to their monocrops
(see Figure 3.4).
Total N yields (corn +
legumes) from plots, where legumes were grown, however, were much higher than N
yields obtained from monocrops of corn at all levels of N application in both
seasons (Figure 3.8 and Appendix Table 4).
Soybean plots had
the highest total N yields. This
suggests that an appreciable amount of N ha-1 can be harvested if legumes
are included in intercropping systems with corn.
Nitrogen yields in
sequential crops of corn in season 2 and season 4 are presented in Figure
3.9. In season 2, N yields of corn
following the grain legumes (22.4 to 25.0 kg ha-1) were higher than
the N yield (19.5 kg ha-1) obtained with 33 kg ha-1
urea-N and lower than the N yield (26.6 kg ha-1) obtained with 67 kg
ha-1 urea-N applied in corn.
N yields
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obtained from the
monocrops and intercrops of legumes were not different in season 2.
In season 4, the N yields of corn following grain legumes were comparable with N yield (29.5 kg ha-1)
obtained with 33 kg N ha-1 in corn; however, the N yields from the monocrops of indeterminate mungbeans
(40.3 kg ha-1) and soybeans (36.5 kg ha-1) were higher
than the N yield (35.9 kg ha-1) from monocropped corn with 67 kg ha-1
of urea N applied. The monocrop of
indeterminate mungbeans provided the highest N yield in both seasons. Higher N yields of corn following indeterminate mungbeans may have been due to higher
% N in root and nodules of indeterminate mungbeans than of determinate
mungbeans (Table 3.11).
Percent N in corn ear
leaves at 50% silking are presented in Table 3.12. Percent N in corn ear leaves in intercrops were comparable with
the % N (1.54) in ear leaves of monocropped corn with 67 kg N ha-1 treatment in season 1 and with the % N (1.09) with 33 kg N ha-1 treatment
in season 3. Except in plots of
monocrop of indeterminate mungbeans, % N in ear leaves of corn following grain
legumes (1.92 to 1.96% in season 2 and
1.76 to 1.91% in season 4) were comparable to
the % N in ear leaves of monocropped corn with 33 kg N ha-1 in seasons 2 and 4. Corn
following the indeterminate mungbean monocrop had the highest % N in ear leaves
(2.25 and 2.17% N in seasons 2 and 4, respectively), which were comparable to % N in ear leaves of monocropped corn with 67 kg N ha-1
treatment.
The % N in ear leaves at
corn in summer (seasons 1 and 3) was
considerably lower than ear
leaf N in winter (seasons 2 and 4) at 4
levels of applied N in corn monocrops (Figure 3.10). This may result from the reduced production of carbohydrates
necessary for growth in winter due to reduced solar radiation. Similar differences in % N in ear leaves of
corn between winter and summer were also reported by Evensen (1983).
An estimate of amounts of
N transferred from grain legumes to corn
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was made comparison with
the uptake of N from four rates of urea-N by corn (Figure 3.11). Based on the N uptake by corn, no N was contributed to corn by legumes in
season 1 and 10 to 25 kg N ha-1 was contributed in season 3 (Table
3.13).
On the basis of N uptake,
the N contributions
from grain legumes to the following corn crop were estimated to be 40
to 58 kg N ha-1 in
season 2 and 31 to 75 kg
N ha-1 in season 4 (Table 3.13). Residual N from legumes taken up by
the following corn crop was the highest from indeterminate mungbean monocrops (58.0 and 75.0
kg N ha-1) followed by soybean monocrops (40.0
and 62.5 kg N ha-1) and determinate mungbean
monocrops (35.0 and 47.0 kg N ha-1). N contributed from legume
monocrops was higher than
that from legume intercrops in both seasons 2 and 4.
These results indicate
that there was very little if any N
contributed to
corn from grain legumes while they were growing together. These results also suggest that legumes and corn did not compete for soil N in an intercropping
situation, however, the residual N from grain legumes to the following crop of corn was substantial.
These results agree with those of other
studies where it was shown that mungbeans (Agboola and Fayemi, 1972; Singh and
Singh, 1975) and soybeans (Shrader et al., 1966; Saxena and Tilak, 1975) were
more beneficial in terms of N supply to cereal crops when grown in rotation
with cereal crops than as a companion crop.
N
Recovery from Urea
The percentages of N recovered by corn from
Urea-N is presented in Table
3.14. The N recovered from urea in
summer plantings were in the ranges of 31 to 49% and 28 to 59% in seasons 1 and
3, respectively, and in winter plantings were in the ranges of 3 to 12% and 26
to 34% in seasons 2 and 4,
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respectively. These results show that appreciably less N was recovered in
winter than in summer. The N recovery
from urea-N was very low in season 2 during which there was heavy rainfall and
low solar radiation that probably accounted for the poor crop of corn in that
season. In the summer, however, N
recovery from urea was comparable to that in other studies where average N
recovery was 50% (Allison, 1966; Soper et al., 1971).
Soil
Nitrogen
Available NH4-N and NO3-N
before and after each season are presented in Appendix Table 8. In the beginning of the experiment, the
available NH4-N and NO3-N in the top 15 cm of soil were low in the ranges of 10.35 to 13.54 ppm and 7.32 to 10.19 ppm,
respectively. The data show that the
availability of NH4-N and NO3-N in the top 15 cm of soil
were higher after seasons 1 and 3, and were lower after seasons 2 and 4. The higher values after seasons 1 and 3 may
have been due to the fact that grain legumes were
grown in seasons 1 and 3, while lower values
after seasons 2 and 4 may have resulted from the upake of N by corn following
legumes. Also the heavy rainfall in
seasons 2 and 4 may have caused N to
be lost by leaching and
denitrification.
Effects on Nitrogen Fixation
Large variations in nitrogenase activity were
observed from season 1 to season 3 (Table 3.15). The nitrogenase activities in mungbeans were not reduced
significantly by intercropping in both
seasons 1 and 3. There were no significant
adverse effect on total nitrogenase activity (TNA) or specific nitrogenase activity (SNA) of intercropped soybeans
compared to monocropped soybeans, except for the significant reduction in mass of nodules/plant of soybeans
in season 1. The reduction in mass of nodules/plant
of soybeans in season 1 may have been due to shading or soybeans by corn
(see Appendix Figure 2).
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The ratios of TNA in monocropped legumes compared to those in intercropped
legumes were 1.3, 1.5 and 1.4 in 1 and 1.0, 0.9 and 0.8 in season 3 for intercrops of determinate mungbeans, indeterminate
mungbeans and soybeans, respectively (calculated from Table 3.15). Higher
ratios in season 1 indicated that
there was a slight (but non-significant) decrease in N2 fixation by
intercropping of legumes in season 1 but lower ratios in season 3 indicate that
intercropping did not adversely affect nitrogenase activity of these two grain
legumes in season 3.
Correlation coefficients
for the relationship between several
variables related to N2 fixation
in mungbeans and soybeans presented
in Table 3.16. Total nitrogenase
activity was significantly correlated
with number of nodules/plant (r values of 0.58 and 0.68 for mungbeans and
soybeans, respectively) and nodule mass/plant (r values of 0.54 and 0.79 for
mungbeans and soybeans, respectively).
The relationship between number of nodules/plant and nodule was also significant with r values of 0.80 in
mungbeans and 0.76 in soybeans. In both
mungbeans and soybeans, the specific nitrogenase activities were negatively
correlated (but not significant at the 0.05 level) with number of nodules/plant
and mass of nodules/plant.
Soybeans had much higher N2 fixing
ability (μ mole
ethylene/plant/-hour of 13.08 to 18.68 in season 1 and 20.93 to 26.43 in season
3) than mungbeans (μ mole ethylene/plant/hour of 2.50 to 4.40 in season 1
and 7.10 to 7.44 in season 3, Table 3.15).
This higher N2 fixation by soybeans may account for the
higher N yields obtained from soybeans as than from mungbeans (Figure 3.8).
N contributions to the succeeding crops of
corn from indeterminate mungbeans (58 to 75 kg ha-1) were higher
than those from soybeans (40.0
to 62.5 kg ha-1, in spite of the
difference in ability to fix N (Table
3.13). One reason for this might be that a greater portion of the fixed N may
have been harvested in the above ground parts of soybeans than in mungbeans
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(Figure 3.8). Also, mungbeans were harvested about 7 weeks earlier than
soybeans (Table 3.2), which may have
allowed more time for mungbean roots and nodules in the soil to decompose and,
therefore, release more N to the succeeding crop of corn.
There was no significant difference in the N2
fixation by indeterminate and by determinate mungbeans (Table 3.15). The N contributions to the succeeding crops of corn
in both seasons 1 and 3, however, were higher from indeterminate hungbeans (58
to 75 kg ha-1) than from determinate mungbeans (31 to 47
kg ha-1, Table 3.13). Since
flowering proceeded over a longer period of time in the indeterminate variety,
the N2 fixation also may have continued for a longer period of time in the indeterminate mungbeans.
Thus the total N2 fixed by
indeterminate mungbeans was higher than that fixed by determinate mungbeans,
which resulted in higher N contributions from
indeterminate mungbeans.
The results suggest that N2 fixation
by mungbeans and soybeans generally was the same whether they were monocropped
or intercropped with corn. Soybeans in season 1 were an exception due to the
heavy shading by corn. The
indeterminate mungbeans provided the largest amount of N to the succeeding crop
of corn.
SUMMARY AND
CONCLUSIONS
Field experiments involving intercropping of
two grain legumes (mungbeans and soybeans) with a main crop of corn were
conducted during four consecutive growing seasons
(June 1981 to January 1983) at Waimanalo Research Station in
Hawaii. In seasons 1 and 3, legumes
were grown with or without corn, while
in seasons 2 and 4, these plots of legumes were succeeded by corn. In addition, corn was also grown as a
monocrop at N rates of 0, 33, 67 and 100 kg ha-1 in each
season. The main thrust of this
investigation was to evaluate the yield potential and N economy of intercropping these two grain legumes with corn.
Grain yields of corn increased when
intercropped with legumes compared to grain yields of corn monocropped without
N application. The increases in
intercropped corn grain yields over monocropped corn grain yields without N
were 158, 163 and 163% in season l, and 181, 146 and 118% in season 3 for
corn/determinate mungbeans, corn/indeterminate mungbeans and corn/soybean
intercrops, respectively. There were no
significant changes in total dry matter, harvest index, and plant height of
corn in intercrops compared to corn monocropped without N.
The grain and total dry matter yields of
mungbeans and soybeans were depressed when intercropped relative to
monocropped. This indicates that the
corn was dominant over legumes when they were growing together. In general, the plant heights, number of
pods/plant and harvest indices of intercropped legumes were not different from
those of monocropped legumes.
The total biomass produced by corn/legume
intercropped treatments (6.11 to 10.88 mg ha-1) were much
higher than the biomass produced by control plots (3.08 to 4.33 Mg ha-1)
of corn. Total grain produced by
corn/legume intercropping systems (1.58 to 3.45 Mg ha-1) were 4 to 6
times higher than the grain produced by control plots of corn (0.39 to 0.55 Mg
ha-1). Total LAI obtained in
corn/legume intercropping systems was higher than the LAI in monocrops of
corn. LER values in these intercropping
systems were 1.9 to 2.2 in season 1 and 1.6 to 1.9 in season 3, indicating the
yield advantages in intercropping over monocropping systems.
In seasons 2 and 4, where corn crops followed
legumes, the overall grain yields were poor due to lower solar radiation and
temperature during the winter season.
Grain yields and plant heights of corn
following legumes were comparable with the grain yields and plant heights of corn monocrops with 33 to 67 kg ha-1 of applied
N. There were no significant
differences in harvest indices among treatments.
Nitrogen yields of intercropped corn were not
different from the N yields of monocropped corn without N in season 1. In season 3, however, the yield of intercropped corn was comparable to
the N yield of monocropped corn which received 33 kg N ha-1. N yields by intercropped legumes were
lower than the N yields by monocropped legumes. Total N yields from corn/legume intercropped treatments, however,
were much higher than N yields from monocropped corn at the maximum rate of applied N (100 kg N ha-1). This suggests that appreciable amounts of N
can be harvested if legumes are intercropped with corn.
In general, N yields of corn following grain
legumes in seasons 2 and 4 were in between the N yields of monocropped corn
fertilized with 33 and 67 kg N ha-1. The N yields of corn following
indeterminate mungbeans and soybeans
in season 4, however, were higher than the N yields of monocropped corn
fertilized with 67 kg N ha-1.
Based on the N uptake by corn, the N
contributions from legumes to the associated corn crop were zero in season 1 and 10 to 25 kg N ha-1 in season
3. N contributions from legumes to following corn, however, were 40 to 58 kg N
ha-1 in season 2 and 31 to 75 kg N ha-1 in season 4.
The residual N contributions to
following corn were highest from indeterminate mungbeans (58.0 to 75.0
kg N ha-1) followed by
soybeans (40.0 to 62.5 kg N ha-1) and determinate mungbeans (35.0 to
47.0 kg N ha-1 ).
The N2
fixation by mungbeans and soybeans was not depressed by intercropping, except
for soybeans in season 1 where soybean win shaded by corn due to narrow row spacing.
On the basis of the
results obtained in this investigation, it can be concluded that corn
intercropped with mungbeans or soybeans may perform better than corn
monocropped without N application.
Furthermore, in areas where food production is the prime objective (as
in most subsistance farming systems), intercropping corn with mungbeans or
soybeans can provide a substantial amount of total grain/ha which can not be
obtained from monocropping corn without N.
It can also be concluded
that there is no or very little transfer of N from mungbeans or soybeans to the
associated corn crop. A substantial
amount of residual N from mungbean or soybean residues, however, can be
utilized by the following corn crop, thus reducing the amount of N input in
cropping systems. In the areas where
the supply at N-fertilizers is limited and/or N-fertilizers are too expensive to be used
by common farmers (as in most of the developing countries), the inclusion of
these legumes in cropping systems may
provide a cheap alternative source of
N.
CHAPTER
IV
FORAGE
LEGUMES WITH OR WITHOUT INTERCROPPING WITH CORN (Zea mays L.).
INTRODUCTION
Forage legumes are grown
with grasses to increase yields as well as to improve the nutritional value of
the forages. In addition to increased
yields and nutritional value, the practice of legume/grass mixtures is based on
the assumption that grasses utilize nitrogen fixed by legumes.
Forage legumes are
included in cropping with food crops. One of the major food crops grown in these cropping is corn. Among the legume forage legumes, leucaena,
because of its multiple uses, is popularly grown with corn. Efforts have been made to grow leucaena with
corn (Mendoza et al., 1975; Guevarra, 1976; IITA, 1979; Rosa et al., 1980; Kang
et al., 1981b; Mendoza et al., 1981).
In a corn/leucaena
intercropping
experiment, no reduction in yield of either crop was observed by Guevarra
(1976). At IITA (1979), corn yields
were higher in the corn/leucaena intercrop (2.8 t ha-1) than in the
corn monocrop (2.5 t ha-1).
In another experiment, grain yields of corn were increased from 48.5 g plant-1
in pure stand to 69.9-74.4 g plant-1 in a corn/leucaena intercrop (Rosa et al.,
1980).
Another forage legume of
importance in the subtropics
is desmodium. Most of the work has been done with desmodium/grass mixtures (Younge et
al., 1974; Whitney et al., 1967; Whitney and Green, 1969; Whitney, 1970). No study has been reported where desmodium
was intercropped with corn.
The amount of N
contributed by a legume to an associated non-legume or to a subsequent crop
basically depends on the N fixing ability and N requirement of the legume. The amount of N fixed by leucaena has been
reported to range from 310 to 800
kg N ha-1 yr-1 (Brewbaker et al., 1972; Gomez and
Zandstra, 1976). Most of the work on N contributions from
leucaena to corn has been done by adding leucaena foliage to corn plots
(Guevarra, 1976; Kang et al., 1981a, 1981b; Read, 1982; Evensen, 1983). No work has been reported on the transfer of
N from leucaena to an associated corn crop or the residual N available from the
root system of leucaena to the following crop of corn.
Desmodium has been found
to fix as much as 381 kg N ha-1 yr-1 and was able to
transfer about 5% of its N to associated grasses (Whitney et al., 1967). Transfer of N from desmodium to associated
grass was also reported to be as little as 1.66% in sand culture (Henzell, 1962) to as much as 20%
to pangolagrass (Whitney and Green, 1969).
An
accumulation of
101 to 112 kg N ha-l yr-1 in soil by desmodium has also
been reported (Henzell et al., 1966).
No work has been reported on the evaluation of N transfer from desmodium
to an
associated corn crop or the residual N available to a subsequent crop of corn.
Legumes differ in their
N fixing abilities and N required for their growth. Since,
leucaena (tree type) and desmodium (creeping type) differ in their growth
patterns, the yield performance and N
contribution to corn
from these legumes may be different. No effort has been made
to compare the performance of these two types of forage crop with corn. Therefore, there is need to further
investigate the use of these
forage legumes (leucaena and desmodium) in cropping systems with corn.
The present investigation
was conducted to evaluate the yield potential and N economy of intercropping two forage
legumes with corn.
MATERIALS
AND METHODS
A field experiment
involving intercropping of two forage legumes (leucaena
and desmodium) with a main crop of coin during four consecutive growing seasons
and a crop of corn following the forage legumes in season 5 was conducted at
Waimanalo Research Station in very fine kaolinitic, isohyperthermic, Vertic
Haplustoll soil.
Planting
Two crops of sweet corn were grown in the field to remove available N from the soil before
starting the experiment. Corn (Zea
mays L.) var. H 763 was grown as a main crop. Leucaena (Leucaena leucocephala (Lam.) de wit) var.
Hawaiian Giant (K8) and desmodium (Desmodium intortum (Mill) Urb)
var. Greenleaf were grown with or
without corn in four consecutive growing seasons. In season 5, leucaena and desmodium stubble were killed by spraying a
50:50 mixture
of Roundup
and Diesel directly
over stubble. Two weeks after spraying,
legume plots were
tilled and corn was planted. In
addition, monocrops of corn were grown at urea-N rates of 0, 33, 67 an a 100 kg
ha-1 in each season. The
experiments were arranged in a randomized block design with 4 replications.
Leucaena seeds were
scarified with sulfuric acid, and then were inoculated with TAL 582 strain of Rhizobium
spp. before planting in dibble tubes on March 27, 1981. Seedlings were watered regularly and a
N-free plant nutrient solution was supplied to the seedlings by drenching every two weeks for about
12 weeks before transplanting in the experimental plots. Desmodium seeds were inoculated with a mixture of TAL
569, TAL 667 and TAL 1147 strains of Rhizobium spp. before
planting.
Planting of desmodium and
transplanting of leucaena were done on June 15, 1981.
Five crops of corn were planted on June 15, 1981, November 10, 1981,
April 22, 1932, September 30, 1982 and February 15, 1983 In seasons 1 through
5, respectively. P as triple super
phosphate and K as muriate of potash were applied at the rates 120 and 100 kg
ha-1,
respectively, for all crops in each
season. N as urea was applied at four levels (0, 33, 67, and 100 kg ha-1)
only in monocrops of corn in each season.
Treatments with monocrops of legumes and intercrops of legumes with corn
were not supplied with N.
Leucaena and desmodium were
planted at plant densities of 50,000 and 800,000 plants ha-1,
respectively, in both monocrop and intercrop. Corn was planted at a density of 53, 333 plants ha-1 in the monocrop
and 40,000 plants ha-1
in the intercrop. Leucaena was planted
in rows 100 cm apart with a within row plant spacing of 20 cm in both the monocrop and intercrop. The row spacing for desmodium was 25 cm and
the plant spacing was 5 cm in both the monocrop and intercrop. Corn was planted in rows 75 cm
apart in the monocrop and 100 cm apart
in the intercrop, and had a plant
spacing of 25 cm in both monocrop and
intercrop. Planting patterns are presented in Appendix Figure l.
Weed and Insect
Control
Atrazine and Lasso
Preemergence herbicides were applied at the rate of 2 kg ha-1 of
each in plots of monocropped corn. In all other legume plots only Lasso was applied at the rate of 2 kg ha-1. Weeds
were also removed by hand whenever necessary.
Diazinon and Sevin (at the rate of 12 oz each
in 100 gallons of water) were sprayed to control the insect, mainly Rose
beetle.
Harvesting
Leucaena and desmodium were harvested at
intervals of 6 to 8 weeks at heights of 50 and 5 cms, respectively. This much
stubble was left for regrowth of these perennials. Leucaena and desmodium both harvested
9 times. Harvest numbers 1 and 2
were made in season 1, harvest numbers 3 and 4 in season 2, harvest 5, 6 and 7 in season 3, and harvest numbers 8 and 9 in season 4.
Plant Height and LAI
Heights of 10 plants from each treatment were measured and the mean values were used for plant height.
Leaf area index of desmodium were measured by
taking leaves from 5 plants in each of the desmodium plots, and then measuring
the leaf area with a Leaf Area Meter (LIOOR-CI - 3100). In leucaena, subsampling of leaves was done
and the leaf areas of these subsamples were
measured. Based on the total dry matter
of leaves in the whole plant, the Values from
subsamples of leaves were used to calculate the
leaf area in the whole plant of leucaena. The leaf area index (LAI) was calculated as leaf area pet unit area of land.
Dry Matter Yield
Grain and stover yields
were measured in corn. Above ground
parts of leucaena and desmodium were measured for forage yields. Total dry matter yields were calculated by the addition of all
components. Yields are reported in
Megagrams per hectare (Mg ha-1), which is a metric ton or million grams per hectare.
Nitrogen Contents
Ear-leaf samples taken
from corn plants at the 50% silking stage
were analyzed for N content.
Grain, stover, and forage samples after each harvest were analyzed for N
content by the Microkjeldahl method (Bremner, 1965a), and total N yields were
calculated.
Soil samples taken from
individual plots, before and after each crop season, were analyzed for
available NH4-N and NO3-N by the
Steam-distillation method
(Bremner, 1965b).
Evaluation
Productivity per hectare
of land was estimated by calculating land equivalent ratios (LER) for all the
intercropped plots. The calculation was
done as:
Corn intercrop yield Legume intercrop yield
LER =
-------------------- + -----------------------
Corn monocrop yield Legume monocrop yield
A harvest index (HI) was
calculated for each crop as HI = economic yield/biological yield, where grain yield was the economic yield and above ground total dry matter was used as
the biological yield.
Nitrogen contributions from legumes to corn
were estimated by comparing the N uptake by intercropped corn with the N uptake
by monocropped corn at four levels of N.
Statistical analysis of the data included the
analysis of variance, F test, Duncan’s multiple range test, simple correlation
technique and regression analysis.
RESULTS AND
DISCUSSION
Performance of Corn in Intercropping
Corn responded well to increased rates of N
application in seasons 1 and 3, which happened to be summer (Figure 4.1). Increases in grain yields of corn were from
0.39 to 4.28 Mg ha-1 in season 1 and from 0.55 to 4.82 Mg ha-1 in season 3 with increased rates
of N application iron 0 to 100 kg ha-1, respectively. Response
to increased rates of N by corn was
poor in seasons 2 and 4, which were the winter period. Grain yields of corn increased from 0.38 to
0.57 Mg ha-1 in season 2 and from 0.39 to 0.99 Mg ha-1 in
season 4 as applied N increased from 0 to 100 kg ha-1, respectively. The poor performance of corn during the
winter (seasons 2 and 4) compared to summer (seasons 1 and 3) was due to lower
solar radiation and temperature during the winter (Appendix Table 3).
Grain yields of corn intercropped with
leucaena and desmodium were not significantly different from the grain yields
of monocropped corn without N in seasons 1, 3 and 4 (Figure 4.2 and Appendix
Table 5); however, grain yield of
corn was significantly depressed in the Leucaena plot in season 2. Percentages of corn grain yields obtained
with intercropping compared to monocropping (control plots) were 128 and 72% in
season 1, 60 and 71% in season 2, 122 and 91% in season 3, and 102 and 118% in
season 4 in leucaena and respectively (Table
4.1). Corn with leucaena seemed to do a little better than with desmodium in
seasons 1 and 3 (summer), while corn with desmodium seemed to do a little
better than corn with leucaena in seasons 2 and 4 (winter). However, these differences were not
significant. Except in season 2, there
seemed to be a slight yield advantage to corn grown with leucaena over
monocropped corn without N, while except in season 4, there seemed to be no
yield advantage to corn grown with desmodium over monocropped corn without N. Again, these differences were not
significant.
Total dry matter yields (grain + stover) of
corn in leucaena and desmodium plots
were not depressed in seasons l,
3 and 4, however, total dry matter
yield of corn was depressed by leucaena in season 2 (Figure 4.2).
Harvest indices of corn intercropped with
leucaena and desmodium were not different from those of the control plots of
corn (Table 4.2). Plant heights of corn
intercropped with leucaena and desmodium were not significantly different from
the plant height of monocropped corn without N in seasons 1 and 3, but were
significantly higher in seasons 2 and 4 (Table 4.2).
The reduction in grain yield and total dry
matter of corn grown with
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leucaena in season 2 was probably the result
of the corn being shaded by leucaena as it was observed that leucaena overgrew
the coal (Appendix Figure 4). Yield
depression in corn in leucaena plot in season 2 suggests that shading effects can be
minimized by better scheduling of intervals for cutting leucaena.
In general, comparable
grain yields can be obtained when corn is intercropped with leucaena or
desmodium to when it is monocropped without N application. These results agree with those of Guevarra
(1976) who found no reduction in corn yield when corn was intercropped with leucaena.
Performance of Forage Legumes
Seasonal dry matter
yields of leucaena and desmodium are presented in Figure 4.3. Forage yields of leucaena intercrops were
slightly reduced in seasons 1 and 2, and were slightly increased in seasons 3
and 4 compared to leucaena monocrops in the respective seasons. Forage yields of leucaena intercrops were
not significantly different from forage yields of leucaena monocrops in all
four seasons. In desmodium, slight
depressions in intercrop yields were observed compared to their monocrop
yields in all four seasons; however, these yield depressions were not
statistically significant (Figure 4.3 and Appendix Table 6). These results indicated that leucaena seemed
to do little better as an intercrop than as a monocrop towards the end of the
experiment, while the opposite was true with desmodium.
Both crops had higher
yields in seasons 1 and 3 (summer) than in seasons 2 and 4 (winter), with the
highest yields in season 3 (Figure 4.3).
In season 1, since leucaena and desmodium both took about 2 to 4
weeks for establishment in the field before making real growth, the yields were
lower than in season 3.
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Over a growing period of
590 days leucaena accumulated 26.16 and 25.07 Mg ha-1 dry matter
when monocropped and intercropped,
respectively (Table 4.3). While,
desmodium in a growing period of 591
days
accumulated 32.81 and
28.64 Mg ha-1 dry matter when monocropped and intercropped,
respectively. Total dry matter
accumulated by the end of this experiment by intercropped and monocropped
leucaena were significantly different; however, there was a reduction of about
4 Mg ha-1 dry matter by desmodium
intercropped compared to monocropped
during this experimental period.
Leucaena had equally good growth in the intercrop as in the
monocrop (Appendix Figure 5). The
reduction in dry matter accumulation by desmodium during the last part of the
experiment may have been due to the death
of some of the desmodium plants during this period.
Annual dry matter yields
of leucaena were 18.14 and 17.82 Mg ha-1 yr-1 in the monocrop and
intercrop, respectively (Appendix Table
7).
The monocrop and
intercrop of desmodium produced 22.46 and 19.70 Mg ha-1 yr-1
respectively. These results suggest
that both forage legumes are capable of producing high amounts of biomass ha-1
yr-1.
Solar radiation,
temperature, dry matter yield for each harvest
and dry matter accumulation per day by leucaena and desmodium are presented in Figure
4.4. Changes in dry matter yields of
leucaena and desmodium in each harvest coincided with changes in solar
radiation. From June to September in
1981, average monthly solar radiation was in the range of 20 to 22 MJ m-2
day-1 and so were yields of first harvest of leucaena and desmodium
in September 1981. Solar radiation declined to a
value of 6.7 MJ m-2 day-1 in October 1981 and remained
low until April 1982 and as a consequence the yields of the second, third, and
fourth harvests of leucaena and desmodium were low. After April 1982, solar radiation increased and remained high
until September 1982 in the
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range of 14.0 to 16.6 MJ m-2 day-1
and yields of leucaena and desmodium were high during that period. After September 1982, solar radiation
declined and so did yields of the last two harvests of leucaena and desmodium.
Dry matter accumulation
(g m-2 day-1) by leucaena and desmodium were affected by changes
in solar radiation (Figure 4.4). Rates of dry matter accumulation were higher during periods of higher
solar radiation (summer) and were lower during periods of lower solar radiation
(winter) in both crops. Rates of dry
matter accumulation by monocrops and intercrops of leucaena were very similar
during the entire growing period. In
desmodium, rates of dry matter accumulation by monocrops and intercrops were very
similar up to harvest number 4, but after that dry matter accumulation was
higher in the monocrops. In leucaena,
the similar dry matter accumulation could have been due to the fact that the growth
of leucaena in the intercrop was as good as in monocrop, since leucaena was
able to compete successfully with corn.
While in desmodium, the reduced dry matter accumulation could have been
due to the death of some of the original plants and thereby a reduced plant
population towards the end of the experiment.
Changes in monthly
average temperature wore similar to the changes in solar radiation during the
period of this experiment. The
correlation coefficient between solar radiation and temperature during the
entire period of 4 seasons was 0.82.
The correlation between solar radiation and yields of leucaena and
desmodium was found to have r values
of 0.71 and 0.88, respectively. At the
same site in another experiment, the correlation between solar radiation and
temperature, and correlation between solar
radiation and yield of leucaena were reported
to be 0.79 and 0.73,
respectively, by Hedge (1983). These
results show
that environmental
conditions have profound effects on the forage yields of leucaena and
desmodium.
Total Performance in Intercropping
Total dry matter yields
of corn/forage legume intercrops compared to dry matter of monocrops of corn are presented in Figure
4.5 and Appendix Table 2. Total dry matter produced in season 1 in corn/forage legume intercrops were
comparable to total dry matter produced by corn at an N rate of 100 kg ha-1. In general, total dry matter produced by corn/forage
legume intercrops in seasons 2, 3 and
4 were higher than dry matter produced by monocrops
of corn fertilized with 100 kg N ha-1. These
results suggest that much higher total biomass can be produced by a
corn/forage legume intercropping system than
by a monocrop of corn with no N application grown under similar
environmental conditions.
LAI’s of corn in
corn/desmodium intercrops were lower than the LAI’s in control plots, while the LAI’s of corn in
corn/leucaena intercrops were
higher than in the control plots (Table 4.4).
The total LAI’s in corn/forage legume
intercrops were 11.83 and 9.61 for monocropped and intercropped
leucaena, respectively, and 3.15 and 3.58 for monocropped and
intercropped desmodium, respectively.
Leucaena had much higher LAI than any
other crop. Higher LAI in corn/legume intercrops compared to control plots of corn may have resulted in higher
interception of the incoming solar radiation in intercropping systems than in
monocropping, and this was the reason for higher biomass production/ha in
intercropping systems.
Land equivalent ratios
(LER) in corn/forage legume intercrops are presented in Table 4.5. Values of LER for corn grown with leucaena
were more than one in all seasons, except season 2, indicating a yield
advantage for corn in all seasons but season 2, when corn was shaded
leucaena. Values of LER for corn grown
with desmodium were lower than one
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in all seasons except season
4, which indicated a yield depression of corn in seasons 1 through 3. The total LER in corn/leucaena and corn/desmodium intercrops, however, were in the ranges of
1.40 to 2.10 and 1.60 to 1.81, respectively.
Except in season 2, LER values from corn/Leucaena intercrops were higher
than from corn/desmodium intercrops in all other seasons. These values of LER indicated that one would
have needed 1.40 to 2.10 hectares and 1.60 to 1.81 hectares of land of
monocrops to produce as much as was produced in one hectare of the
corn/leucaena and corn/desmodium intercrops, respectively.
These results indicated that much higher production/ha
could be achieved by corn/forage legume intercrops than by monocrops of corn
with no N application. In those areas where N fertilizers are in
short
supply and/or are too
expensive for a common farmer
to use, the use of corn/forage legume intercropping systems may be a reasonable
and inexpensive alternative to obtain food as well as forage yields without
inputs of inorganic N.
N Yield and Transfer
Total N yields by
monocrops of corn and corn/forage legume intercrops in all 4 seasons are
presented in Figure 4.6 and Appendix Table 4. N yields
of corn intercropped with leucaena and desmodium were not significantly
different from the N yields obtained from monocropped of corn without N
application in all 4 seasons.
Based on the N uptake by
corn (Figure 3.11), N contributions from legumes to corn were nil in seasons 1
and 2, while N contributions to corn were 30 and 17 kg N ha-1 in season
3, and 19 and 9 kg N ha-1 in season 4 from leucaena and desmodium
respectively. These result suggest that
practically no N was transferred from forage legumes to corn in seasons 1 and 2 but there was N transfer
in season 3 and 4. These N
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contributions in seasons
3 and 4 may have been due to N accumulations over a period of time in corn/legume plots.
Soil nitrogen analysis
indicates that NH4-N and NO3-N in the forage legume plots at the beginning of the
experiment were low in the ranges of 11.47 to 13.06
and 8.60 to 10.35 ppm, respectively (Appendix Table 8).
After season 4, however, the available N as NH4 and NO3
in forage legume plots increased 2 to 3 times in the ranges of 31.59 to 38.22
and 15.29 to 25.48 ppm,
respectively. The increase in NH4-N
and NO3-N was probably due
to the accumulation of N over a period
in these forage legume plots.
Based on N accumulation
during several periods, average N yields from leucaena were 653 and 630 kg ha-1 yr-1
in monocrops and intercrops, respectively (Appendix Table 7). From desmodium average N yields were 608 and
508 kg ha-1 yr-1 in monocrops and intercrops
respectively. Other studies reported N
yields of 310-800 kg ha-1 yr-1 in leucaena (Brewbaker et
al., 1973; Gomez and Zandstra, 1976) and 381 kg ha-1 yr-1 in desmodium (Whitney
et al., 1967). These results suggest
that N production/ha can be greatly increased, if these forage legumes are
included in cropping systems.
Total N yields obtained
in corn/legume plots were
considerably higher than in control plots or even in monocrops of corn at 100 kg ha-1
of applied N. During the period of this
investigation, total N yields obtained from corn/leucaena intercrops were 7 to
21 times higher than the N yields obtained from control plots of corn, and that from corn/desmodium intercrops were 7 to 14
times higher than the N yields obtained from the control plots of corn (Appendix Table 4).
These high N yields from
intercropping are likely due to the high content in leucaena and desmodium leaves (Appendix Table 6). The N content in leucaena and desmodium
foliage ranged from 3.84 to 4.39% and 2.38 to 2.85%, respectively. The % N in foliage in both forage legumes was slightly higher in winter (seasons 2 and 4) than in the
summer (seasons 1 and 3). Similar higher
% N in leucaena in winter than
in summer was reported by Hegde (1983).
The dry matter and N
yields were highly correlated in both leucaena (r = 0.89 to 0.99) and desmodium (r = 0.79 to 0.98) crops
in all 4 seasons (Table 4.6). Since
there were higher dry matter yields during the summer, more N
was incorporated with carbon to make other
compounds, and, therefore, the % N was lower in summer than in winter. This may also be the reason
for the negative (but non-significant) r values
between dry matter and %
N in foliage during the summer. The
opposite may occur during the winter.
Performance of Corn Following
Forage Legumes
In season 5, grain yields of corn (monocrops)
increased linearly from 0.55 to 3.03 Mg ha-1 as N rates were increased from 0 to 100 kg N ha-1 (Figure 4.7). The slope of the regression line shows that with each additional
kg of N, the predicted increase in corn grain yield would be about 26 kg.
The performance of corn following forage
legumes in season 5 is presented in Table 4.7.
Plant heights of corn following forage legumes were higher than in the
control plot (1286 mm) and were comparable to the plant height (1710 mm) of corn obtained with 33 kg ha-1 applied N.
Grain yields of corn
obtained in legume plots (1.22 to 1.43 Mg ha-1 in leucaena plots and 1.29 to 1.52 Mg ha-1 in desmodium plots) were higher
than grain yield in the control plot (0.55 Mg ha-1) and were
comparable to grain yield of corn obtained with 33 kg ha-1 of
applied N (1.32 Mg ha-1).
Total dry matter yields showed similar
trends as those of corn grain
yields. Only the harvest index
of the control plot was
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significantly different
from those of other treatments (Table 4..7).
Percent N in corn leaves
at 50% silking and N yields of corn following forage legumes were also
comparable with % N in corn leaves (1.10%) and N yield (19.5 kg ha-1)
obtained with N application of 33 kg ha-1 (Table 4.7).
The N uptake by corn
increased linearly with increased rates of N, with an R2 of 0.82
(Figure 4.8). The regression coefficient predicts that with each additional kg of N about 0.42 kg of N uptake by corn may
be expected, which also means that
the efficiency of applied urea-N was 42%.
Based on this regression
(Figure 4.8), the N contributions from forage
legumes to the succeeding crop of corn were estimated
to be
21 to 31 kg ha-1 from leucaena
and 23 to 30 kg ha-1 from
desmodium.
These results suggested that in season
5, where desmodium stubble was killed and all the roots and stubble were incorporated into the soil, the crop of corn
received 23 to 30 kg N ha-1 from decomposition of stubble and roots.
In leucaena plots, where leucaena stubble was killed (but not incorporated into the soil and the roots were not
disturbed), the succeeding crop of
corn received 21 to 31 kg ha-1.
It is
possible that the leucaena roots being
thick and woody may have not decomposed fast enough to supply
most of their N to succeeding crop; therefore, only a part of the N
from leucaena roots may have been available to the succeeding corn crop and still more N may have been
released into soil with further decomposition of roots after the corn was harvested.
SUMMARY AND
CONCLUSIONS
A field experiment involving intercropping of
two forage legumes (leucaena and desmodium) with a crop of
corn was conducted during four
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consecutive growing seasons beginning in June
1981 at Waimanalo Research Station in Hawaii.
In season 5, leucaena and desmodium were followed by corn. The main
objective of this investigation was to
evaluate the
yield potential and N economy of
intercropping these two forage legumes with corn.
Grain yields of corn
intercropped with leucaena were
slightly higher than in control plots in all seasons except season 2, where
corn was shaded by leucaena. Grain yields
of corn intercropped with leucaena were 128, 60, 122, and 102% of
control plots in seasons 1 to 4, respectively.
While grain yields of corn with desmodium were slightly lower than the control
plots in all seasons except season 4. Grain yields of corn intercropped with desmodium
were 72, 71, 91, and 118% of control plots in seasons 1 to 4,
respectively. In general, corn did
better with leucaena than with desmodium.
However, corn seemed to perform better with leucaena than
with desmodium during summer and better with desmodium than with leucaena
during winter times.
Seasonal forage yields of leucaena and
desmodium were not significantly different in intercrops as compared to monocrops. Leucaena did somewhat better as intercrop than as monocrop
towards the end of the experiment
while the opposite was true in case of desmodium. On an annual basis forage
yields produced by desmodium (19.7 to 22.5 Mg ha-1 yr-1)
were higher than forage yields of leucaena (17.6 to 18.1 Mg ha-1
yr-1). The environment had large effects on the seasonal yields of forages.
The total biomass produced by corn/forage legume
intercropped plots (4.5 to 17.0 Mg ha-1) were much higher than the
biomass produced by control plots (3.08 to 4.33 Mg ha-1)of corn. Total Leal Area Index in corn/legume intercropping systems
(9.61 in corn/leucaena
and 3.58 in corn/desmodium) were much higher than the LAI in control plots at
corn (1.57). Total Land Equivalent Ratios in
corn/leucaena and corn/desmodium intercrops were in the range of 1.40 to 2.10 and 1.60 to 1.81, respectively. LER values greater than one clearly
indicated the yield advantages in intercropping over monocropping systems.
Nitrogen yields of corn
intercropped with leucaena and desmodium were not different from the N obtained in
control plots in all 4 seasons. On
an average, N produced by leucaena were from 630 to 653 kg ha-1 yr-1
and by desmodium were from 508 to 608 kg
ha-1 yr-1. Total N yields obtained from corn/leucaena intercroppings
were 7 to 21 times and from corn/desmodium intercroppings were 7 to 14 times as
much the N yields obtained from control plots of corn. This suggest that an appreciable amount of N ha-1 can be harvested
if these legumes are included in the cropping systems.
Based on the N uptake by
corn, there was no N contributions from legumes to associated corn in seasons 1
and 2; however, there was some N contribution from legumes to associated corn
in seasons 3 and 4 (19 to
30 kg N ha-1
from leucaena and 9 to 17 kg N ha-1 from desmodium). Corn
following forage legumes
in season 5 received
residual N
of 21 to 31 kg
ha-1 from
leucaena plots and 23 to 30 kg ha-1 from desmodium plots.
On the basis of the
results obtained in this investigation, it can he concluded that in general
corn intercropped with leucaena performed better than monocropped corn with no
N application. There was a slight
reduction in corn yield when intercropped with desmodium. Total productivity/ha in corn/forage legume intercropping, however,
was much higher than in monocropped
corn.
It can be concluded that
there is no or very little N transfer from leucaena or desmodium to the
associated corn crop, however, a substantial amount of residual N from leucaena
and desmodium residues can be utilized by the following crop of corn, thus
reducing the proportionate amount of N input required in cropping systems. In those areas where land size is small and
the supply of N-fertilizers is limited (as in most developing countries), the
inclusion of these forage legumes in cropping systems may provide an alternative source of N and at the same time may provide both food and forage from the same piece of land.
CHAPTER V
EVALUATION OF
LEUCAENA (Leucaena leucocephala (Lam.) de wit)
AS A GREEN LEAF
MANURE FOR CORN (Zea mays L.)
INTRODUCTION
Green manuring has been in practice from
ancient times and at the present is becoming of increasing importance due to
the increasing costs and unavailability of nitrogenous fertilizers in many
parts of the world.
Leucaena with its capacity for fixing high
amounts of atmospheric nitrogen (310 to 800 kg N ha-1 yr-1)
and high N content (3 - 4%) in its foliage (Brewbaker et al., 1972; Gomez and
Zandstra, 1976) is becoming popular for its use as green-leaf manure. Two basic types of systems involving
leucaena use as a green manure are being practiced. In the first, hedgerows of leucaena are intercropped with food
crops, also known as “alley cropping”, where leucaena foliage are periodically
pruned and mulched or incorporated into the soil for use by the companion food
crop. The second system involves sole
cropping of leucaena, where leucaena foliage is cut and carried to another
field where it is mulched or incorporated into the soil for use by another food
crop. The latter one is also known as a
“cut and carry” system.
In a corn/leucaena intercropping experiment,
where leucaena foliage was incorporated into the soil, the yield of
intercropped corn with leucaena incorporation was comparable to yield of corn
where urea was applied at the rate of 75 kg N ha-1 (Guevarra,
1976). In a corn/leucaena alley
cropping experiment, application of 100 kg ha-1 of fertilizer N, 10
t ha-1 of leucaena prunings, or 50 kg ha-1 of fertilizer
N plus 5 t ha-1 of leucaena pruning treatments produced 4.5, 3.7,
and 3.5 t grain ha-1, respectively, in contrast to 2.6 t
ha-1 for the no N control (Kang et al., 1981a). Increased corn grain yields with application
of leucaena pruning over control plot (no N applied) were also reported in
other experiments (Kang et al., 1981b; Mendoza et al., 1981).
In cut and carry system, Read (1982) studied
several important leucaena green-leaf manure management alternatives and
reported that fresh-leaf application was better than dry-leaf application,
incorporation of leucaena was better than mulching, and there was no difference
in applying the leucaena at planting and splitting the application over
time. In Hawaii, Evensen (1983)
reported that incorporation of leucaena leaves was superior to mulching.
In chapter IV, where leucaena was
intercropped with corn for forage purpose and leucaena prunings were not
applied into the soil, N contribution from leucaena to companion corn crop was
not significant. Therefore, further
investigation on the use of leucaena forage as a green manure to corn crop is needed
to understand the full potential of leucaena as a N source.
The main objectives of the present
investigation were to : 1) evaluate the use of leucaena as a green-leaf manure
in corn production, 2) compare the efficiency of leucaena green-leaf manure
with urea as N sources, and 3) determine residual effects of leucaena
green-leaf manure on the following crop of corn.
MATERIALS AND METHODS
A field experiment involving green manuring
of leucaena to corn was conducted during two consecutive growing seasons
begining June 1982 at Waimanalo Research Station in a very fine, kaolinitic,
isohyperthermic Vertic Haplustoll soil.
Treatments
The experiment was arranged in a randomized
complete block design with 7 treatments and 4 replications. Treatments applied were a control plot (no N
applied), three levels of urea-N application (33, 67, and 100 kg N ha-1)
and three levels of leucaena-N application (47, 94, and 141 kg N ha-1).
Planting
Two plantings of corn (var. H 763) were made
in this investigation. The first
planting was made on June 3, 1982 to evaluate the potential of leucaena forage
as a green manure to the corn crop and the second
planting was made on September 30, 1982 to
evaluate the residual effects of leucaena green manure. Spacing of 75 cm between rows and 25 cm
between plants were used to give a planting density of 53,333 plants ha-1
in both seasons.
Leucaena var. Hawaiin Giant (k8) was used as
a green manure to corn. Succulent leaf and stem portions of leucaena forage
were cut and carried from another field to the corn plots. Leucaena forage was chopped and then 5.78,
11.56, and 17.25 kg of chopped leucaena (air dried to 15% moisture and 2.84% N)
were applied per 30 m2 plot in the field for 47, 94, and 141 kg
leucaena-N ha-1, respectively.
Leucaena forage was incorporated into the top 15 cm of the soil by
rotary tiller one week before planting of the first crop of corn. No leucaena
forage was applied to the second crop of corn.
Urea-N was applied at three levels (33, 67,
and 100 kg N ha-1) in both seasons. P as triple super phosphate, and K, as
muriate of potash were applied at the rates of 120 and 100 kg ha-1,
respectively, in all plots in both seasons.
The first and the second crops of corn were
harvested on September 23, 1982 and January 24, 1983, respectively. Sampling area at the time of harvest was
6.75 m2 in both corn crop.
Observations
Plant heights of 10 plants from each
treatment were measured after silking and mean values were used.
Grain and stover yields were measured. Total dry matter production was calculated
by addition of all the components.
Yields are reported in Megagrams per hectare (Mg ha-1), which
is a metric ton or a million grams per hectare.
Harvest index (HI) was calculated as:
HI = economic yield/biological yield,
where grain yield was the economic yield and
the above ground total dry matter was used as the biological yield.
Ear leaf samples taken from corn plants at
the 50% silking stage in each season were analyzed for N content. Grain and stover samples taken after each
harvest were analyzed for N content by Microkjeldahl method (Bremner, 1965a),
and total N yields was calculated. Soil
samples taken from individual plots before and after each crop season were
analyzed for available NH4-N and NO3-N by
steam-distillation method (Bremner, 1965b).
Nitrogen recoveries from the applied urea-N
and leucaena-N were calculated in both seasons as:
N uptake by plants N uptake by plants
with added N ---- with no N added
% N recovery=
-------------------------------------------
Rate of N applied
Evaluation
Two methods were used to evaluate the
potential of leucaena forage as green manure to corn: 1) by comparing corn
grain yields in leucaena-N vs urea-N treatments, and 2) by comparing N uptake
by corn plants in leucaena-N vs urea-N.
For statistical analysis an analysis of
variance of the data was conducted. F
tests, Duncan’s multiple range tests, simple correlation techniques and
regression analysis were used wherever necessary.
RESULTS AND
DISCUSSION
Performance of Corn in Season 1
Plant heights of corn increased with
increasing rates of urea-N and leucaena-N (Table 5.1). Plant height of corn at leucaena-N
application of 47 kg ha-1 was comparable with plant height obtained
at urea-N application of 33 kg ha-1, and plant heights of corn at
leucaena-N rates of 94 and 141 kg ha-1 were comparable with plant
height obtained at urea-N rate of 67 kg ha-1.
Corn grain yields increased from 0.51 to 3.72
Mg ha-1 as urea-N rates were increased from 0 to 100 kg N ha-1
(Table 5.1). Corn grain yield (1.03 Mg
ha-1) obtained at leucaena-N rate of 47 kg N ha-1 was
higher than that of control plot (0.51 Mg ha-1). Corn grain yields obtained at leucaena-N
rates of 94 and 141 kg N ha-1 were comparable with grain yields
obtained at urea-N rates of 33 and 67 kg ha-1, respectively. Total dry matter of corn had the same trend
as observed for corn grain yield.
Harvest indices of corn increased with increasing rates of urea-N. Harvest indices of corn from leucaena
incorporated plots (0.20 - 0.27) were comparable with the harvest index (0.26)
of corn from the plot where urea-N was applied at the rate of 33 kg N ha-1.
Leucaena green manuring at the rates of 47,
94, and 141 kg N ha-1 produced corn grain yields equivalent to
urea-N application rates of 18, 35, and 58 kg N ha-1, respectively
(Table 5.1 and Figure 5.1). The
efficiency of leucaena green manures to produce corn grain as compared to
urea-N applications were found to be 37 to 41% in season 1. In other words, corn with application of 100
kg of leucaena-N might be able to produce grain
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yields as much as produced by application of
37 to 41 kg of urea-N. These values
agree with the results of Guevarra (1976) who reported that the efficiency of
leucaena-N applied to corn was about 38% of that of urea. The results of this investigation suggested
that 37 to 41 kg of urea-N could be saved by green manuring corn with 100 kg of
leucaena-N.
Nitrogen yields and percent N in plant
tissues of corn in season 1 are presented in Table 5.2. Nitrogen yields of corn increased from 19.7
to 65.2 kg ha-1 as the urea-N rates were increased from 0 to 100 kg
N ha-1. N yields of corn
also increased from 34.0 to 58.4 kg N ha-1 with increasing rates of
leucaena-N from 47 to 141 kg N ha-1. N yields obtained at the leucaena-N rates of 47, 94, and 141 kg N
ha-1 were comparable with N yields obtained at the urea-N rates of
33, 67, and 100 kg N ha-1, respectively.
Percent N in corn ear leaves at 50% silking
stage increased from 0.92 to 1.75% as the urea-N rates were increased from 0 to
100 kg N ha-1 (Table 5.2).
Percent N in corn ear leaves of leucaena green manure plots at the rates
of 47, 94, and 141 kg N ha-1 were comparable with % N in corn ear
leaves of urea applied plots at the rates of 0, 33, and 67 kg N ha-1,
respectively. In general, the % N in corn grain decreased with increasing rates
of N application, which may have been due to the dilution factor.
Based on the Figure 5.2, the leucaena green
manuring at the rates of 47, 94, and 141 kg N ha-1 produced N yields
equivalent to urea-N rates of 34, 54, and 90 kg N ha-1,
respectively. The efficiency of
leucaena green manures to increase N yields of corn compared to urea-N
applications were found to be 57 to 72%.
In other words, corn with application of 100 kg of leucaena-N might be
able to produce N yields as much as produced by the application of 57 to 72 kg
of urea-N.
Performance of Corn in Season 2
Plant height of corn increased with
increasing rates of urea-N from 0
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to 100 kg N ha-1 (Table 5.3). Plant heights of corn from the plots, where
leucaena green manures were applied in the previous season (season 1), were
slightly higher than the plant height of corn in control plot but were not
significant.
Corn grain yield increased from 0.34 to 1.24
Mg ha-1 as urea-N rates were increased from 0 to 100 kg N ha-1
(Table 5.3). Corn grain yield (0.46 Mg
ha-l from the plot where leucaena green manure was applied at the
rate of 47 kg N ha-1 in the previous season was higher than the corn
yield (0.34 Mg ha-1) from the control plot. Corn grain yields from the plots of
previously green manured plots at the rates of 94 kg N ha-1 (0.56 Mg
ha-1) and 141 kg N ha-1 (0.63 Mg ha-1) were
comparable with grain yield obtained urea-N rate of 33 kg N ha-1
(0.61 Mg ha-1). Total dry
matter of corn obtained from the previously green manured plots were in between
the total dry matter obtained from the control plot and from the plot of urea-N
rate of 33 kg N ha-1.
Harvest indices of corn obtained from previously green manured plots
were comparable with the harvest index of corn at urea-N rate of 33 kg N ha-1.
In season 2, the response of corn to N
application was poor (Figure 5.3). The
slope of the regression line showed that with addition of every kg of N the
expected increase in corn grain yield was only 9 kg in season 2 (Figure 5.3),
while it was 31 kg in season 1 (Figure 5.1).
The poor response of corn in season 2 was due to the fact that this was
the winter and lower solar radiation and lower temperature were available to
corn as compared to season 1 which happened to be summer season.
Based on the Figure 5.3, the corn grain
yields obtained in season 2 from the leucaena green manured plots in season 1
at the rates of 47, 94, and 141 kg N ha-1 were equivalent to urea-N
application rates of 13.0, 24.5, and 30.5 kg N ha-1,
respectively. These results indicated
that the residual effects of leucaena green manures from season 1 were
equivalent to 13.0 to 30.5 kg ha-1 of urea-N in season 2.
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Nitrogen yields of corn increased from 16.9
to 40.9 kg ha-l with increasing rates of urea-N from 0 to 100 kg N
ha-1 in season 2. N yields
obtained in season 2 (20.2 to 23.9 kg N ha-1) from the previously
green manured plots were comparable with the N yield (24.1 kg ha-l)
obtained at the urea-N rate of 33 kg N ha-l. Percent N in corn ear leaves at 50% silking
from previously green manured plots were in between the % N in corn ear leaves
at urea-N rates of 33 and 67 kg N ha-l. In general, the % N in corn grain decreased with increasing rates
of urea-N. Percent N in corn grain from
previously green manured plots were in between the % N in corn grain at urea-N
rates of 67 and 100 kg N ha-1.
The N uptake by corn was poor with increasing
rates of urea-N in season 2 (Figure 5.4).
The slope of the regression line showed that with addition of every kg
of N the expected increase in N uptake by corn was only 0.24 kg in season 2
(Figure 5.4), while it was 0.44 kg in season 1 (Figure 5.2). The poor uptake of N by corn in season 2 was
due to poor growth of plant during the winter time as compared to better growth
of plant during season 1 (summer time).
The N uptake by corn in season 2 from the
leucaena green manured plots in season 1 at the rates of 47, 94, and 141 kg N
ha-l were equivalent to urea-N rates of 13.5, 22.0, and 30.0, respectively
(Table 5.4 and Figure 5.4). These results of N uptake by corn indicated that
residual effects of leucaena green manures from season 1 were equivalent to
13.5 to 30.0 kg N ha-1 of urea-N in season 2. Based on the corn grain yields, the similar
residual effects of leucaena green manures were found to be equivalent to
urea-N rates of 13.0 to 30.5 kg ha-1 (Figure 5.3).
Nitrogen Recovery
Recovery of N from urea-N applied to corn
varied from 39.4 to 47% in season 1 and 22 to 24.3% in season 2 (Table 5.5). Better plant growth during
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summer (season 1) compared to winter (season
2) may have been the reason for higher N recovery by corn in season 1 as
compared to season 2. Also, the higher
rainfall during season 2 as compared to season 1 may have caused leaching of N
into soil, thus making N partly unavailable to corn plants (Appendix Table 3).
Recoveries of N from leucaena-N applied to
corn were 26.3 to 30.5% in season 1 (Table 5.5). Recoveries of residual leucaena-N in season 2 were 5.0 to 7.1%. Thus, the total N recovered from the
leucaena-N applied were 31.7 to 37.6% by two crops of corn. These results of recovery of leucaena-N
agree with the leucaena-N recovery (31.7%) reported by Evensen (1983).
Correlations
The correlation matrix of different variables
affecting grain yield and N yield of corn are presented in Table 5.6. All components of corn yield were positively
and significantly correlated among themselves in both season 1 and season 2. All the components of corn yield were positively
correlated with N yield and % N in corn ear leaves but were negatively
correlated with % N in corn grain in both seasons. As discussed earlier, the grain yield and the N yield of corn
increased with increasing rates of urea-N, while the % N in grain decreased
with increasing rates of N application (Table 5.2 and Table 5.4). This negative correlation between % N in grain
and yield components clearly explains the above mentioned trend.
SUMMARY AND
CONCLUSIONS
A field experiment involving green manuring
of leucaena to corn was conducted during two consecutive growing seasons at
Waimanalo Research Station. The first
planting of corn was made to evaluate the potential of leucaena forage as a
green manure to corn crop and the second planting was
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made to evaluate the residual effects of
leucaena green manure. Treatments
applied were a control plot (no N applied), three levels of urea-N application
(33, 67, and 100 kg N ha-1) and three levels of leucaena-N
application (47, 94, and 141 kg N ha-1).
Plant heights of corn increased with
increasing levels of Leucaena-N application in season 1. Corn grain yields obtained from the leucaena
green manuring at the rates of 47, 94, and 141 kg N ha-1 were
equivalent to corn grain yields obtained from urea-N rates of 18, 35, and 58 kg
N ha-1, respectively. The
efficiency of leucaena green manures to increase corn grain yield as compared
to urea-N applications were found to be 37 to 41%.
Nitrogen yields of corn from the leucaena
green manure at the rates of 47, 94, and 141 kg N ha-1 were
equvalent to those of at urea-N application rates of 34, 54, and 90 kg N ha-1,
respectively. The efficiency of
leucaena green manure to increase N yields of corn as compared to urea-N
applications were 57 to 72% in season 1.
In season 2, where residual effects of
leucaena green-leaf manure were evaluated, plant heights of corn from the
previously green manured plots were not significantly different from that of
the control plot. Corn grain yields in
season 2 from the previously green manured plots at the rates of 47, 94, and
141 kg N ha-1 were equivalent to those of urea-N application rates
of 13.0, 24.5, and 30.5 kg N ha-1, respectively. N yields of corn in season 2 from the
previously green manured plots at the rates of 47, 94, and 141 kg N ha-1
were equivalent to those of urea-N application rates of 13.5, 22.0, and 30.0
kg N ha-1, respectively.
Recoveries of N from urea-N were 39.4 to 47%
and from leucaena-N were 26.3 to 30.5% in season 1. Recoveries of residual leucaena-N in season 2 were 5.0 to
7.1%. The total N recovered from the
applied leucaena green manure were 31.7 to 37.6% by two crops of corn.
On the basis of the results obtained in this
investigation, it can be concluded that leucaena forage was 37 to 41% as efficient
in increasing corn grain yield as was urea.
The residual effects of leucaena green manure to the following crop of
corn were equivalent to urea-N application rates of 13 to 30 kg N ha-1. A total of 31.7 to 37.6% of N from the
leucaena green manure was recovered by two crops of corn.
It can be concluded that leucaena can very
well be used as a green manure in cropping systems involving food
production. In the areas where the
supply of N-fertilizers is limited (as in most developing countries), the use
of leucaena as a green manure may provide an alternative source of N and
thereby reduce the dependency on costly commercial N-fertilizers.
CHAPTER VI
NITROGEN UPTAKE BY
WHEAT CROPS FROM 15N-LABELED
LEGUME PLANT
MATERIALS
INTRODUCTION
The increasing cost of nitrogenous
fertilizers has increased the importance and accelerated the use of legume
crops in various cropping systems.
Legumes crops may contribute N to associated non-legumes, to succeeding
non-legumes, or when used as green manure crops for non-legumes. The N
contribution from legume to non-legumes, however, seems more likely to
succeeding non-legumes or when legume residues are recycled into the soil
rather than direct transfer from legumes to companion crops of non-legumes
(Whitney and Kanehiro, 1967; Misra and Misra, 1975; Simpson, 1976; Henzell and
Vallis, 1977).
Not all the organic N added into the soil is
mineralized or is readily available to the companion or succeeding crops. A range of 30-60% of the N in legume residues
has been reported to mineralize and become available for the succeeding crops
and the remainder may be lost or may be incorporated in the soil organic matter
(Bartholomew, 1965; Henzell and Vallis, 1977).
The recovery of N by crops as affected by plant species, soil, climate,
and management practices has been reviewed by Allison (1965; 1966).
Recovery of N by crops can be estimated by
difference and isotopic tracer methods.
The difference method assumes that mineralization, immobilization, and
other N transformations are the same for both fertilized and unfertilized
soils. Obviously, this is an erroneous
assumption which can result in large discrepancies between recoveries
calculated by non isotopic and isotopic techniques. On the other hand, the isotopic tracer method assumes that: 1)
the isotope composition of the tracer is constant; 2) living organisms can
distinguish one isotope from another of the same element only with difficulty;
and 3) the chemical identity of isotopes is maintained in biochemical systems. Although these assumptions are not entirely
valid for all experimental conditions, they may be considered valid for most
studies in which 15N compounds are used as tracers (Hauck and
Bremner, 1976).
The use of 15N-tracers has made it
possible to study the proportion of N derived from different sources. 15N-tracer techniques have also
been used in studies dealing with evaluation of uptake of N from plant residues
(Yaacob and Blair, 1980; Herridge, 1982).
Yaacob and Blair (1980) using 15N-labeled soybeans and
siratro residues reported that rhodesgrass recovered 14.6 to 16.8% of N from
soybeans and 13.7 to 55.5% of N from siratro.
Herridge (1982) reported that only 11 to 17% of the 15N-labeled
medicago residues added to the soil were utilized by a succeeding wheat crop,
while 72-78% remained in the soil organic pool.
In a recent study, Ladd et al. (1983) using 15N-labeled
Medicago littoralis reported the N recoveries of 20.2 to 27.8% of the
legume N applied by the first crop of wheat and only 4.8% by the second crop of
wheat. The proportion of wheat N
derived from added legume N was 52-65% for grain and 5-6% for roots.
In chapter III, among the legumes tested, the
indeterminate mungbeans had the highest N contribution to the succeeding crop
of corn. No report has been found to show the N recovery by non-legumes from
mungbean residues with the use of 15N-tracers.
The experiment reported here was an attempt
to evaluate the N recovery by two crops of wheat from 15N-labeled
mungbean plant materials applied into the soil.
MATERIALS AND METHODS
Tagging of Mungbeans
An indeterminate mungbean crop (Vigna radiata)
cultivar v 2013 was grown on October 29, 1982 in 3-gallon pots having a 50:50
mixture of soil and vermiculite in the greenhouse. A total of 152.10 g of 15N-labeled ammonium sulfate
(60-85% enrichment) containing 23 g of 15N was applied equally in
100 pots (1.521 g of ammonium sulfate in each pot) in solution form. Pots were watered regularly and water
leached from the pots was recycled into the pots.
Initially 12 mungbean plants were grown in
each pot and two weeks later they were thinned to 6 plants per pot. Removed plants were returned into the
pots. Mungbean plants were harvested 60
days after planting at the late flowering and early pod formation stage.
Shoot and root portions of mungbeans were
separated, dried and ground. Ground samples of shoot and root were analyzed for
% N by the Microkjeldhal method.
(Bremner, 1965a) and for atom % 15N by the mass
spectrometer.
Treatments
This greenhouse experiment was arranged in a
randomized complete block design with 17 treatments in 6 replications. Treatments were control (0 N), 4 levels of
urea-N (33, 67, 100, and 200 kg N ha-1), 6 levels of mungbean shoot
-N (33, 67, 100, 200, 300, and 400 kg N ha-1), 3 levels
of mungbean root-N (33, 67, and 100 kg N ha-1) and 3 levels of
mungbean shoot + root-N (33, 67, and 100 kg N ha-1). Based on the N content of the mungbean shoot
(2.5%) and mungbean root (1.5%), the amounts of plant materials applied for
these treatments are presented in Table 6.1.
In addition, P as triple super phosphate, and K, as muriate of potash
were applied at the rates of 100 and 80 kg ha-1, respectively,
to all the treatments.
The soil used in this pot experiment was a
very fine, kaolinitic, isohyperthermic family of Vertic Haplustoll. On the dry weight basis, 7.5 kg of soil per
3-gallon pot and 2.5 kg of soil per 1-gallon pot.
Treatments of mungbean shoot and shoot + root
were applied in 3-gallon pots, but, because of the limited supply of root
materials from mungbeans, root treatments were applied in 1-gallon pots. The rates of N applied (kg N ha-1)
were kept the same for the root treatments, but the size of pot, amount of soil
pot-1 and the number of plants pot-1 were reduced to one
third of the other treatments applied in 3-gallon pots. Assumptions were made that there was no
effect of pot size as the amount of soil, nutrients, and water applied per
plant were the same in all pots.
Planting of Wheat
The first crop of wheat (Triticum aestivum),
cultivar Pavon 76, was planted on January 23, 1983. Initially 12 plants were planted in each of the 3-gallon pots and
4 plants in each of the 1-gallon pots.
Two weeks later plants were thinned to 6 plants in each 3-gallon pot and
2 plants in each 1-gallon pot.
The second crop of wheat was planted on May
16, 1983 to evaluate the residual effect of mungbean plant materials applied
for the first crop of wheat. Plants per
pot and all other managements were kept the same as for the first crop of
wheat.
Harvesting
The first and the second crops of wheat were
harvested at the maturity stage on April 25, 1983 and August 9, 1984,
respectively.
Grain and straw portions of wheat were
separated, dried, and then grain, straw and total dry matter yields per pot
were recorded. Data from root-N
treatments were multiplied by three to make comparisons with other shoot-N and
shoot + root-N treatments.
Grain and straw samples were ground and then
analyzed for % N by Microkjeldahl method (Bremner, 1965a) and for atom % 15N
by mass spectrometer.
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Evaluation
Using regression analysis, two methods were
used to evaluate the N supply from mungbean-N to wheat: 1) by comparing wheat
dry matter yields in mungbean-N vs. urea-N treatments, and 2) by comparing N
uptake by
wheat plants in mungbean-N vs. urea-N
treatments.
Percentage recovery of mungbean-N by wheat
crops was calculated by the following methods:
1. Difference method
(Nf = Nc)
% N recovery =
--------------- X 100,
R
where,
Nf = total N
in the plant from N applied pots,
Nc = total N
in the plant from control pots, and
R = amount of N applied
per pot.
2. Isotopic 15N method
Nf (A-B)
% N recovery =
-------------- X 100,
(C-B) R
where,
Nf = total N
in the plant from mungbean-N applied pots,
A = atom % 15N
in the plant from mungbean-N applied pots,
B = atom % 15N
in the plant from control pots,
C = atom % 15N
in mungbeans applied,
R = rate of mungbeans-N
applied, and
(A-B)
------ x 100 = % of N
uptake by wheat derived from mungbean.
(C-B)
The data from the pot
experiment were analyzed using analysis of variance suited to randomized
complete block design. Specific
treatment comparisons were made by Duncan’s Multiple Range test at the 5%
significance level. Regression analysis
were used wherever necessary.
RESULTS AND
DISCUSSION
Yield of Wheat Crop 1
Grain, straw, and total dry matter yields of
the first crop of wheat increased with increasing rates of urea-N and
mungbean-N (Figure 6.1). Straw yields
of wheat were higher than grain yields at all levels and from all sources of N
applications. Increases in grain and
straw yields of wheat were almost parallel as N rates were increased from 0 to
100 kg N ha-l of urea-N, root-N and shoot + root-N, and from 0 to
200 kg N ha-1 of shoot-N.
When urea-N rates were increased from 100 to 200 kg N ha-1
and shoot-N from 200 to 400 Kg ha-1, the increases in straw yields
were much higher than the increases in grain yields.
The above results suggested that at the lower
levels of N application, there were almost proportional increases in grain and
straw yields, however, at the higher levels of N application (in this case
urea-N beyond 100 kg N ha-1
and shoot-N beyond 200 kg N ha-1), the increase in grain yield was
at slower rate than that of straw, indicating the utilization of major
proportion of photosynthates by straw.
Grain yield of wheat from the highest rate
(400 kg N ha-1) of shoot-N treatment (15.43 g pot-1) was
comparable with urea-N rate of 200 kg N ha-1 (14.02 g pot-1)
(Figure 6.1 and Appendix Table 9).
Grain yields from N rates of 100 kg N ha-1 of shoot-N (8.59 g
pot-1), of root-N (7.65 g pot-1) and of shoot + root-N
(8.13 g pot-1) were comparable with each other and were in between
the grain yields obtained from urea-N rates of 33 and 67 kg N ha-1.
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Total dry matter yields of wheat increased
linearly with increasing rates of urea-N (Figure 6.2). Using this regression line, the dry matter
yields from shoot-N rates of 300 and 400 Kg N ha-1 were comparable
with dry matter yield (39.9 g pot-1) obtained from urea-N rate of
200 kg N ha-1. Dry matter
yields from 100 kg N ha-1 rates of shoot-N, root-N, and shoot +
root-N were comparable with each other (Appendix Table 9) and all these yields
were comparable to yield (19.1 g pot-1) obtained from 33 kg N ha-1
rate of urea-N (Figure 6.2).
All these results indicated that in terms of
dry matter yield of wheat, incorporation of shoot-N was little better than
root-N. The performance of wheat from
various sources of N applications can also be seen in Appendix Figure 6.
Nitrogen Uptake by Wheat Crop 1
Nitrogen uptake by wheat increased with
increasing rates of N applications from all sources (Figure 6.3). Unlike the dry matter yields, where straw
yields were higher than grain yields (Figure 6.1), the N uptake by grain was
higher than that of straw at all levels and from all sources of N (Figure
6.3). This higher N uptake by grain was
as a result of higher % N in grain as compared to straw (Appendix Table 10).
Total N uptake by wheat increased linearly as
the urea-N rates were increased from 0 to 200 kg N ha-1 (Figure
6.4). Using this regression line, the N
uptake by wheat from 100 kg N ha-1 rates of shoot-N, root-N, and
shoot + root-N were equivalent to N uptake by wheat from 33 kg N ha-1
rate of urea-N (0.178 g N pot-1).
As discussed earlier on the basis of dry matter yields (Figure 6.2), the
results from 100 kg N ha-1 rates of shoot N, root-N, and shoot +
root-N were also found to be equivalent to urea-N rate of 33 kg N ha-1. A highly significant correlation (r = 0.95)
was found between the total dry matter and total N uptake by the first crop of
wheat.
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Although not significantly different, in
general, the N uptake by wheat from shoot-N treatments were higher than that of
root-N treatments (Appendix Table 10).
At the same rate of N application (kg N ha-1), the
decomposition and availability of N from shoot may have been higher than from
root, and therefore, wheat from shoot-N treatments may have performed better
than from root-N treatments.
Yields of Wheat Crop 2
Residual effects of mungbean-N on the second
crop of wheat are presented in Table 6.2.
In general, grain, straw, and total dry matter yields of wheat crop 2
were much lower than those of wheat crop 1.
As observed in the first crop of wheat, the grain yields of the second
crop of wheat were also lower than the straw yields at all levels and from all
sources of N. Except the dry matter
yields from shoot-N rates of 300 and 400 kg N ha-1, the dry matter
yields obtained from all other mungbean-N treatments were not different among
themselves. Only the yields obtained
from 100 to 400 kg N ha-1 rates of shoot-N and 100 kg N ha-1 rates
of root-N and shoot + root-N were higher than that of control plot.
Dry matter yield of wheat crop 2 increased
linearly as the urea-N rates were increased from 0 to 200 kg N ha-1 (Figure
6.5). Using this regression line, the
residual effects from 300-400 kg N ha-1 of shoot-N treatments were
equivalent to urea-N rates of 67 kg N ha-1 and the residual effects
from all other mungbean-N treatments were lower than urea-N rate of 33 kg N ha-1.
Nitrogen Uptake by Wheat Crop 2
The N uptake and % N in grain of the second
crop of wheat were higher than in straw at all levels and from all sources of N
(Table 6.3). Total N uptake by the
second crop of wheat was also much lower than the N uptake by the first crop of
wheat. N uptake by the second crop of
wheat were similar
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from 100 kg N ha-1 rates of all
there sources of mungbean-N treatments.
Except the N uptake by wheat from shoot-N rates of 100 to 400 kg N ha-1
and 100 kg N ha-1 rates of root-N and shoot + root-N, the N uptake
from all other residual mungbean-N treatments were not different among
themselves and were not higher than that of control plot. This suggests that the residual effects of N
were observed only at and above 100 kg N ha-1 rate of mungbean-N
application.
N uptake by the second crop of wheat
increased linearly as the urea-N rates were increased from 0 to 200 kg N ha-1
(Figure 6.6). Using this regression
line, the residual effect from 400 kg N ha-1 rate of shoot-N was
equivalent to urea-N rate of 67 kg N ha-1. Except the 300 and 400 kg N ha-l rates of shoot-N, the
residual effects from all other mungbean-N treatments were lower than urea-N
rate of 33 kg N ha-1.
These results of residual effects based on N
uptake (Figure 6.6) agree with the results based on dry matter yield (Figure
6.5). Also a highly significant
correlation (r = 0.96) was found between the total dry matter and total N
uptake by the second crop of wheat.
Nitrogen Recovery by Wheat
Atom % 15N in grain and
straw of wheat increased with increasing rates of shoot, root, and shoot +
root-N (Appendix Table 11). As
expected, atom % 15N in plant tissues of the first crop
of wheat was higher than that of in the second crop of wheat. Atom % 15N in shoot,
root, and shoot + root of mungbean applied were 19.9129, 17.1152, and 18.5140%,
respectively.
Based on the atom % 15N in
plant tissues of wheat, the calculated values of wheat N derived from decomposing
mungbean plant materials by crop 1 and crop 2 are presented in Figure 6.7. Wheat N derived from decomposing mungbean-N
by crop 1 increased with increasing rates of mungbean-N, reaching 70.4% at 400
kg N ha-1 rate of shoot-N, 22.1.% at 100 kg N ha-1 rate
of root-N,
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and 38.0% at 100 kg N ha-1 rate of
shoot + root-N. Except the shoot-N
treatments beyond the rate of 200 kg N ha-1, the increase in wheat N
derived from mungbean applied was proportionate to the increasing rates of
mungbean-N. This suggest that wheat
crop could use the mungbean-N applied proportionately at lower rates below 200
kg N ha-1, however, at the higher rate beyond the 200 kg N ha-1
of mungbean-N, the first crop of wheat was not able to use N proportionately as
the supply of N was far beyond the need of wheat crop.
At a given rate of mungbean-N applied, the N
derived by the first crop of wheat was always higher from shoot-N than from
root-N treatments (Figure 6.7). As
discussed earlier, at the same given rate of mungbean-N, the N uptake by the
first crop of wheat from shoot-N treatments were also higher than that of from
root-N (Appendix Table 10). The
decomposition of shoot may have been faster than roots, and therefore, may have
been readily available to the first crop of wheat.
In general, the N derived from decomposing
mungbean residues by the second crop of wheat was lower than the first crop of
wheat (Figure 6.7). Wheat N derived from residual mungbean-N was highest
(43.5%) from the highest shoot-N rate of 400 kg N ha-1. At a given rate of 100 kg N ha-1,
the residual N derived by the second crop of wheat were similar for shoot-N
(13.7%), root-N (13.7%) and shoot + root-N (14.9%). These results suggested that the residual N available to the
second crop of wheat was lower from lower rates of all sources of N, however,
the residual N was still high at the high rates of N (200-400 kg N ha-1).
N recoveries by the first and the second
crops of wheat estimated by isotopic method and difference method are presented
in Table 6.4. By isotopic method, the N
recoveries by the first crop of wheat were in the range of 15.1-33.9,
11.1-12.0, and 13.8-18.9% from shoot-N (33 to 400 kg N ha-1), root-N (33 to 100 kg N ha-1)
and shoot + root-N (33 to 100 kg N ha-1),
Figure
6.7. Nitrogen derived by two crops of
wheat from mungbean
plant materials and soils.
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respectively. These results indicated that the N recovery by the first crop of
wheat increased as the shoot-N and shoot + root-N rates were increased;
however, there was not much change in N recovery as root-N was increased from
33 to 100 kg N ha-1, and also the N recovery from root-N was the
lowest.
As estimated by the isotopic method, the N
recoveries by the second crop of wheat from residual N of shoot (3.9-5.2%),
root (2.9-4.1%) and shoot + root (4.3-4.7%) were much lower than the N
recoveries by the first crop of wheat (Table 6.4). The N recoveries by the second crop of wheat were not much
different from the all levels and all sources of residual mungbean-N.
Based on the isotopic method, total N
recoveries by two crops of wheat were in the ranges of 19.0-39.2, 14.8-15.3,
and 18.4-23.6% from shoot-N, root-N, and shoot + root-N treatments,
respectively (Table 6.4). At a given N
rate, the total N recovery from shoot-N was higher than from root-N.
As estimated by difference method, the N
recoveries by the first crop of wheat from shoot-N (25.5-44.8%), root-N
(24.4-26.0%), and shoot + root-N (24.2-32.7%) were higher than those estimated
by the isotopic method (Table 6.4). N
recoveries by the second crop of wheat (2.4-9.9%) were also lower than the
first crop as estimated by the difference method, however, these values again
were higher than the values obtained by the isotopic method (2.9-5.2%). Total N recoveries by the two crops of wheat
as estimated by the difference method from shoot-N (31.1-51.6%), root-N
(26.8-33.6%), and shoot + root-N (32.8-41.0%) were also higher than the values
estimated by the isotopic method. In
all the cases, the N recoveries estimated by the difference method were higher
than those by the isotopic method.
These results agree with the other works (Legg and Allison, 1959;
Westerman and Kurtz, 1974), where also the difference method overestimated the
N recovery as compared to isotopic method.
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SUMMARY AND
CONCLUSIONS
A greenhouse experiment was conducted where 15N-tagged
mungbean plant materials as shoot, root and shoot + root were applied to a
wheat crop at the N rates of 0 to 400, 0 to 100, and 0 to 100 kg N ha-1,
respectively. In addition, pots with 5
levels of urea-N (0, 33, 67, 100 and 200 kg N ha-1) were also grown
with wheat crop. A second crop of wheat
was grown to estimate the residual effects of mungbean-N applied.
Total dry matter yields and total N uptake by
the first crop of wheat increased with increasing rates of mungbean-N. Total dry matter yields and total N uptake
by wheat crop 1 obtained from 100 kg N ha-1 rates of shoot-N,
root-N, and shoot + root-N were comparable with those of from urea-N rate of 33
kg N ha-1.
Total dry matter yields and total N uptake by
the second crop of wheat were much lower than those of the first crop of
wheat. Except the higher rates of
mungbean-N applied (at and above 100 kg N ha-1), the residual
effects from all other mungbean-N treatments were not different from the
control plot. The residual effects from
100 kg N ha-1 rates of all sources of mungbean-N were equivalent to
lower than urea-N rate of 33 kg N ha-1.
In both the wheat crops, straw overyielded
the grain at all levels and from all sources of N applied. In contrast, N uptake by grain was higher
than by straw in both wheat crops.
Wheat N derived from mungbean-N increased
with increasing rates of mungbean-N applied and were higher (10.9-70.4%) by the
first crop of wheat and lower (5.4-43.5%) by the second crop of wheat.
Most of the mungbean-N applied was recovered
by the first crop of wheat (11.1-33.9%) and only less than 6% of the N was
recovered by the second crop of wheat.
These results also indicated that recovery of
N was higher from shoots than from roots.
Out of the two methods used to estimate N recovery, the difference
method overestimated the N recovery over the isotopic method.
On the basis of the above results, it can be
concluded that mungbean plant residues can very well be used as N source to
reduce N input for non-legume. The
results indicate that mungbean shoot may be slightly better than root in terms
of immediate N supply to non-legumes; however, in a practical situation, where
mungbeans are harvested for grain and only root portions are left in the soil,
the mungbean root can still reduce the substantial amount of N input for
non-legumes.
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Appendix Figure 1. Planting
Patterns of crops in:
A. monocrops, B. intercrops.
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Appendix Figure 2. Growth
of soybeans
in: A) monocrop,
B) intercrop in season 1
(shaded), and C)
intercrop in season 3
(not shaded).
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Appendix Figure 3. Growth
of determinate mungbeans
as A) monocrop and B) intercrop,
and
of indeterminate
mungbeans as C)
monocrop and D)
intercrop.
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Appendix Figure 5. Growth
of leucaena A) monocrop and
B) intercrop, and desmodium C) monocrop
and D) intercrop.
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Appendix Figure 6. Growth
of wheat crop l at various
rates of A) urea-N, B)
mungbean shoot-N,
C) root-N, and D) shoot + root-N
applications.
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