Nitrogen Dynamics of Grain Legume-Weedy Fallow-Flooded Rice Sequences in the Tropics

Dry‐season (DS) grain legume‐weedy fallow‐wet‐season (WS) flooded rice is a common cropping sequence in the rainfed lowlands of tropical Asia. To better manage N in this cropping system, we need to understand N dynamics and balances as influenced by the aerobic‐anaerobic soil aeration sequence, legu...

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Main Authors: George, Thomas, Ladha, Jagdish K., Garrity, Dennis P., Torres, Rolando O.
Format: Journal Article
Language:Inglés
Published: Wiley 1995
Subjects:
Online Access:https://hdl.handle.net/10568/167381
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author George, Thomas
Ladha, Jagdish K.
Garrity, Dennis P.
Torres, Rolando O.
author_browse Garrity, Dennis P.
George, Thomas
Ladha, Jagdish K.
Torres, Rolando O.
author_facet George, Thomas
Ladha, Jagdish K.
Garrity, Dennis P.
Torres, Rolando O.
author_sort George, Thomas
collection Repository of Agricultural Research Outputs (CGSpace)
description Dry‐season (DS) grain legume‐weedy fallow‐wet‐season (WS) flooded rice is a common cropping sequence in the rainfed lowlands of tropical Asia. To better manage N in this cropping system, we need to understand N dynamics and balances as influenced by the aerobic‐anaerobic soil aeration sequence, legume cropping, biological N2 fixation (BNF), and recycling of legume residues. To understand N dynamics under a range of N derived from BNF (15N‐estimated), harvested in pods and left in residues, we conducted a 2‐yr experiment on a Philippine Alfisol using cowpea [Vigna unguiculata (L.) Walp.], mungbean [V. radiata (L.) Wilcz.], nodulating and nonnodulating soybean [Glycine max (L.) Merr.], and weeds. The main portion of soil mineral N (0 to 60 cm) was NO3 in the dry season and NH4 in the wet season. The sum of soil NO3 and soil N uptake at legume harvest exceeded the decrease in soil NO3 from legume seeding to harvest by 81 kg ha−1, indicating the continued production and legume uptake of soil NO3. The large differences in total N of legumes (46 to 238 kg N ha−1), however, were associated with differences in N derived from BNF (0 to 176 kg N ha−1). When pod N was excluded, legume N balance was, in most cases, negative. The average soil N depletion was 40 kg ha−1 from nonnodulating soybean, compared with 8 kg ha−1 from N2‐fixing legumes. In terms of WS rice grain and N yields, legume cropping did not differ from weedy fallowing, despite greater (by up to 46 kg N ha−1) quantities of legume residue N in some instances. Large amounts of legume residues, however, were associated with reduced legume grain yields, thus decreasing the harvestable grain N output. Fertilizer N, compared with residue N, had a greater effect on WS rice grain and N yields. The use of legumes in lowland rice‐based cropping systems must maximize harvestable N while effectively using soil, BNF, and applied N sources.
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spelling CGSpace1673812024-12-22T05:45:01Z Nitrogen Dynamics of Grain Legume-Weedy Fallow-Flooded Rice Sequences in the Tropics George, Thomas Ladha, Jagdish K. Garrity, Dennis P. Torres, Rolando O. nitrogen nitrogen balance nitrogen fixation cropping systems legumes weeds flooded rice tropics Dry‐season (DS) grain legume‐weedy fallow‐wet‐season (WS) flooded rice is a common cropping sequence in the rainfed lowlands of tropical Asia. To better manage N in this cropping system, we need to understand N dynamics and balances as influenced by the aerobic‐anaerobic soil aeration sequence, legume cropping, biological N2 fixation (BNF), and recycling of legume residues. To understand N dynamics under a range of N derived from BNF (15N‐estimated), harvested in pods and left in residues, we conducted a 2‐yr experiment on a Philippine Alfisol using cowpea [Vigna unguiculata (L.) Walp.], mungbean [V. radiata (L.) Wilcz.], nodulating and nonnodulating soybean [Glycine max (L.) Merr.], and weeds. The main portion of soil mineral N (0 to 60 cm) was NO3 in the dry season and NH4 in the wet season. The sum of soil NO3 and soil N uptake at legume harvest exceeded the decrease in soil NO3 from legume seeding to harvest by 81 kg ha−1, indicating the continued production and legume uptake of soil NO3. The large differences in total N of legumes (46 to 238 kg N ha−1), however, were associated with differences in N derived from BNF (0 to 176 kg N ha−1). When pod N was excluded, legume N balance was, in most cases, negative. The average soil N depletion was 40 kg ha−1 from nonnodulating soybean, compared with 8 kg ha−1 from N2‐fixing legumes. In terms of WS rice grain and N yields, legume cropping did not differ from weedy fallowing, despite greater (by up to 46 kg N ha−1) quantities of legume residue N in some instances. Large amounts of legume residues, however, were associated with reduced legume grain yields, thus decreasing the harvestable grain N output. Fertilizer N, compared with residue N, had a greater effect on WS rice grain and N yields. The use of legumes in lowland rice‐based cropping systems must maximize harvestable N while effectively using soil, BNF, and applied N sources. 1995-01 2024-12-19T12:57:20Z 2024-12-19T12:57:20Z Journal Article https://hdl.handle.net/10568/167381 en Wiley George, Thomas; Ladha, Jagdish K.; Garrity, Dennis P. and Torres, Rolando O. 1995. Nitrogen Dynamics of Grain Legume-Weedy Fallow-Flooded Rice Sequences in the Tropics. Agronomy Journal, Volume 87 no. 1 p. 1-6
spellingShingle nitrogen
nitrogen balance
nitrogen fixation
cropping systems
legumes
weeds
flooded rice
tropics
George, Thomas
Ladha, Jagdish K.
Garrity, Dennis P.
Torres, Rolando O.
Nitrogen Dynamics of Grain Legume-Weedy Fallow-Flooded Rice Sequences in the Tropics
title Nitrogen Dynamics of Grain Legume-Weedy Fallow-Flooded Rice Sequences in the Tropics
title_full Nitrogen Dynamics of Grain Legume-Weedy Fallow-Flooded Rice Sequences in the Tropics
title_fullStr Nitrogen Dynamics of Grain Legume-Weedy Fallow-Flooded Rice Sequences in the Tropics
title_full_unstemmed Nitrogen Dynamics of Grain Legume-Weedy Fallow-Flooded Rice Sequences in the Tropics
title_short Nitrogen Dynamics of Grain Legume-Weedy Fallow-Flooded Rice Sequences in the Tropics
title_sort nitrogen dynamics of grain legume weedy fallow flooded rice sequences in the tropics
topic nitrogen
nitrogen balance
nitrogen fixation
cropping systems
legumes
weeds
flooded rice
tropics
url https://hdl.handle.net/10568/167381
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AT garritydennisp nitrogendynamicsofgrainlegumeweedyfallowfloodedricesequencesinthetropics
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