Transformations and recovery of residue and fertilizer nitrogen15 in a sandy Lixisol of West Africa

The fate of 15N-labeled plant residues from different cover-cropping systems and labeled inorganic N fertilizer in the organic, soil mineral, microbial biomass and soil organic matter (SOM) particle-size fractions was investigated in a sandy Lixisol. Plant residues were from mucuna (legume), lablab (legume), imperata (grass), maize (cereal) and mixtures of mucuna or lablab with imperata or maize, applied as a surface mulch. Inorganic N fertilizer was applied as 15N-(NH4)2SO4 at two rates (21 and 42 mg N kg–1 soil). Total N release from mucuna or lablab residues was 2–3 times higher than from the other residues, whereas imperata immobilized N throughout the study period. In contrast, 15N was mineralized from all the plant residues irrespective of the mineralization–immobilization pattern observed for total N. After 168 days, 69% of soil mineral N in mucuna- or lablab-mulched soils was derived from the added residues, representing 4–8% of residue N, whereas 9–30% of inorganic N was derived from imperata, maize and the mixed residues. At the end of the study, 4–19% of microbial biomass N was derived from the added residue/fertilizer-N, accounting for 1–3% of added residue-N. Averaged across treatments, particulate SOM fractions accounted for less than 1% of the total soil by weight but contained 20% of total soil C and 8% of soil N. Soils amended with mucuna or lablab incorporated more N in the 250–2000 μm SOM pool, whereas soil amended with imperata or the mixed residues incorporated similar proportions of labeled N in the 250–2000 μm and 53–250 μm fractions. In contrast, in soils receiving the maize or inorganic fertilizer-N treatments, higher proportions of labeled N were incorporated into the 53–250 μm than the 250–2000 μm fractions. The relationship between these differences in residue/fertilizer-N partitioning into different SOM particle-size fractions and soil productivity is discussed.

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Main Authors: Ibewiro, B., Vanlauwe, Bernard, Sanginga, P., Merckx, R.
Format: Journal Article biblioteca
Language:English
Published: 2000
Subjects:cropping systems, soil, fertilizers, maize,
Online Access:https://hdl.handle.net/10568/99913
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spelling dig-cgspace-10568-999132023-06-12T21:03:14Z Transformations and recovery of residue and fertilizer nitrogen15 in a sandy Lixisol of West Africa Ibewiro, B. Vanlauwe, Bernard Sanginga, P. Merckx, R. cropping systems soil fertilizers maize The fate of 15N-labeled plant residues from different cover-cropping systems and labeled inorganic N fertilizer in the organic, soil mineral, microbial biomass and soil organic matter (SOM) particle-size fractions was investigated in a sandy Lixisol. Plant residues were from mucuna (legume), lablab (legume), imperata (grass), maize (cereal) and mixtures of mucuna or lablab with imperata or maize, applied as a surface mulch. Inorganic N fertilizer was applied as 15N-(NH4)2SO4 at two rates (21 and 42 mg N kg–1 soil). Total N release from mucuna or lablab residues was 2–3 times higher than from the other residues, whereas imperata immobilized N throughout the study period. In contrast, 15N was mineralized from all the plant residues irrespective of the mineralization–immobilization pattern observed for total N. After 168 days, 69% of soil mineral N in mucuna- or lablab-mulched soils was derived from the added residues, representing 4–8% of residue N, whereas 9–30% of inorganic N was derived from imperata, maize and the mixed residues. At the end of the study, 4–19% of microbial biomass N was derived from the added residue/fertilizer-N, accounting for 1–3% of added residue-N. Averaged across treatments, particulate SOM fractions accounted for less than 1% of the total soil by weight but contained 20% of total soil C and 8% of soil N. Soils amended with mucuna or lablab incorporated more N in the 250–2000 μm SOM pool, whereas soil amended with imperata or the mixed residues incorporated similar proportions of labeled N in the 250–2000 μm and 53–250 μm fractions. In contrast, in soils receiving the maize or inorganic fertilizer-N treatments, higher proportions of labeled N were incorporated into the 53–250 μm than the 250–2000 μm fractions. The relationship between these differences in residue/fertilizer-N partitioning into different SOM particle-size fractions and soil productivity is discussed. 2000 2019-03-03T05:54:02Z 2019-03-03T05:54:02Z Journal Article Ibewiro, B., Vanlauwe, B., Sanginga, P. & Merckx, R. (2000). Transformations and recovery of residue and fertilizer nitrogen-15 in a sandy Lixisol of West Africa. Biology and Fertility of Soils, 31(3-4), 261-269. https://hdl.handle.net/10568/99913 en Limited Access p. 261-269
institution CGIAR
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-cgspace
tag biblioteca
region Europa del Oeste
libraryname Biblioteca del CGIAR
language English
topic cropping systems
soil
fertilizers
maize
cropping systems
soil
fertilizers
maize
spellingShingle cropping systems
soil
fertilizers
maize
cropping systems
soil
fertilizers
maize
Ibewiro, B.
Vanlauwe, Bernard
Sanginga, P.
Merckx, R.
Transformations and recovery of residue and fertilizer nitrogen15 in a sandy Lixisol of West Africa
description The fate of 15N-labeled plant residues from different cover-cropping systems and labeled inorganic N fertilizer in the organic, soil mineral, microbial biomass and soil organic matter (SOM) particle-size fractions was investigated in a sandy Lixisol. Plant residues were from mucuna (legume), lablab (legume), imperata (grass), maize (cereal) and mixtures of mucuna or lablab with imperata or maize, applied as a surface mulch. Inorganic N fertilizer was applied as 15N-(NH4)2SO4 at two rates (21 and 42 mg N kg–1 soil). Total N release from mucuna or lablab residues was 2–3 times higher than from the other residues, whereas imperata immobilized N throughout the study period. In contrast, 15N was mineralized from all the plant residues irrespective of the mineralization–immobilization pattern observed for total N. After 168 days, 69% of soil mineral N in mucuna- or lablab-mulched soils was derived from the added residues, representing 4–8% of residue N, whereas 9–30% of inorganic N was derived from imperata, maize and the mixed residues. At the end of the study, 4–19% of microbial biomass N was derived from the added residue/fertilizer-N, accounting for 1–3% of added residue-N. Averaged across treatments, particulate SOM fractions accounted for less than 1% of the total soil by weight but contained 20% of total soil C and 8% of soil N. Soils amended with mucuna or lablab incorporated more N in the 250–2000 μm SOM pool, whereas soil amended with imperata or the mixed residues incorporated similar proportions of labeled N in the 250–2000 μm and 53–250 μm fractions. In contrast, in soils receiving the maize or inorganic fertilizer-N treatments, higher proportions of labeled N were incorporated into the 53–250 μm than the 250–2000 μm fractions. The relationship between these differences in residue/fertilizer-N partitioning into different SOM particle-size fractions and soil productivity is discussed.
format Journal Article
topic_facet cropping systems
soil
fertilizers
maize
author Ibewiro, B.
Vanlauwe, Bernard
Sanginga, P.
Merckx, R.
author_facet Ibewiro, B.
Vanlauwe, Bernard
Sanginga, P.
Merckx, R.
author_sort Ibewiro, B.
title Transformations and recovery of residue and fertilizer nitrogen15 in a sandy Lixisol of West Africa
title_short Transformations and recovery of residue and fertilizer nitrogen15 in a sandy Lixisol of West Africa
title_full Transformations and recovery of residue and fertilizer nitrogen15 in a sandy Lixisol of West Africa
title_fullStr Transformations and recovery of residue and fertilizer nitrogen15 in a sandy Lixisol of West Africa
title_full_unstemmed Transformations and recovery of residue and fertilizer nitrogen15 in a sandy Lixisol of West Africa
title_sort transformations and recovery of residue and fertilizer nitrogen15 in a sandy lixisol of west africa
publishDate 2000
url https://hdl.handle.net/10568/99913
work_keys_str_mv AT ibewirob transformationsandrecoveryofresidueandfertilizernitrogen15inasandylixisolofwestafrica
AT vanlauwebernard transformationsandrecoveryofresidueandfertilizernitrogen15inasandylixisolofwestafrica
AT sangingap transformationsandrecoveryofresidueandfertilizernitrogen15inasandylixisolofwestafrica
AT merckxr transformationsandrecoveryofresidueandfertilizernitrogen15inasandylixisolofwestafrica
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