Managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in Kenya

In sub-Saharan Africa, maize is one of the most important staple crops, but long-term maize cropping with low external inputs has been associated with the loss of soil fertility. While adding high-quality organic resources combined with mineral fertilizer has been proposed to counteract this fertility loss, the long-term effectiveness and interactions with site properties still require more understanding. This study used repeated measurements over time to assess the effect of different quantities and qualities of organic resource addition combined with mineral nitrogen (N) on the change of soil organic carbon (SOC) contents over time (and SOC stocks in the year 2021) in four ongoing long-term experiments in Kenya. These experiments were established with identical treatments in moist to dry climates, on coarse to clayey soil textures, and have been conducted for at least 16 years. They received organic resources in quantities equivalent to 1.2 and 4 t C ha−1 yr−1 in the form of Tithonia diversifolia (high quality, fast turnover), Calliandra calothyrsus (high quality, intermediate turnover), Zea mays stover (low quality, fast turnover), sawdust (low quality, slow turnover) and local farmyard manure (variable quality, intermediate turnover). Furthermore, the addition of 240 kg N ha−1 yr−1 as mineral N fertilizer or no fertilizer was the split-plot treatment. At all four sites, a loss of SOC was predominantly observed, likely because the sites had been converted to cropland only a few decades before the start of the experiments. Across sites, the average decline of SOC content over 19 years in the 0 to 15 cm topsoil layer ranged from 42 % to 13 % of the initial SOC content for the control and the farmyard manure treatments at 4 t C ha−1 yr−1, respectively. Adding Calliandra or Tithonia at 4 t C ha−1 yr−1 limited the loss of SOC contents to about 24 % of initial SOC, while the addition of sawdust, maize stover (in three of the four sites) and sole mineral N addition showed no significant reduction of SOC loss over the control. Site-specific analyses, however, did show that at the site with the lowest initial SOC content (about 6 g kg−1), the addition of 4 t C ha−1 yr−1 farmyard manure or Calliandra with mineral N led to a gain in SOC contents. The other sites lost SOC in all treatments, albeit at site-specific rates. While subsoil SOC stocks in 2021 were little affected by organic resource additions (no difference in three of the four sites), the topsoil SOC stocks corroborated the results obtained from the SOC content measurements (0–15 cm) over time. The relative annual change of SOC contents showed a higher site specificity in farmyard manure, Calliandra and Tithonia treatments than in the control treatment, suggesting that the drivers of site specificity in SOC buildup (soil mineralogy, soil texture, climate) need to be better understood for effective targeting management of organic resources. Farmyard manure showed the highest potential for reducing SOC losses, but the necessary quantities to build SOC are often not realistic for smallholder farmers in Africa. Therefore, additional agronomic interventions such as intercropping, crop rotations or the cultivation of crops with extended root systems are necessary to maintain or increase SOC.

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Main Authors: Laub, Moritz, Corbeels, Marc, Couedel, Antoine, Ndungu, Samuel Mathu, Mucheru-Muna, Monicah Wanjiku, Mugendi, Daniel, Necpalova, Magdalena, Waswa, Wycliffe, Van de Broek, Marijn, Vanlauwe, Bernard, Six, Johan
Format: article biblioteca
Language:eng
Subjects:F08 - Systèmes et modes de culture, P33 - Chimie et physique du sol, fumier, agroécosystème, Zea mays, ressource minérale, carbone, Tithonia, séquestration du carbone, engrais organique, teneur en éléments minéraux, stockage, matière organique du sol, fertilité du sol, carbone organique du sol, http://aims.fao.org/aos/agrovoc/c_2810, http://aims.fao.org/aos/agrovoc/c_36669, http://aims.fao.org/aos/agrovoc/c_8504, http://aims.fao.org/aos/agrovoc/c_4852, http://aims.fao.org/aos/agrovoc/c_1301, http://aims.fao.org/aos/agrovoc/c_32257, http://aims.fao.org/aos/agrovoc/c_331583, http://aims.fao.org/aos/agrovoc/c_4592, http://aims.fao.org/aos/agrovoc/c_4848, http://aims.fao.org/aos/agrovoc/c_7427, http://aims.fao.org/aos/agrovoc/c_35657, http://aims.fao.org/aos/agrovoc/c_7170, http://aims.fao.org/aos/agrovoc/c_389fe908, http://aims.fao.org/aos/agrovoc/c_4086,
Online Access:http://agritrop.cirad.fr/608540/
http://agritrop.cirad.fr/608540/1/ID608540.pdf
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id dig-cirad-fr-608540
record_format koha
institution CIRAD FR
collection DSpace
country Francia
countrycode FR
component Bibliográfico
access En linea
databasecode dig-cirad-fr
tag biblioteca
region Europa del Oeste
libraryname Biblioteca del CIRAD Francia
language eng
topic F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
fumier
agroécosystème
Zea mays
ressource minérale
carbone
Tithonia
séquestration du carbone
engrais organique
teneur en éléments minéraux
stockage
matière organique du sol
fertilité du sol
carbone organique du sol
http://aims.fao.org/aos/agrovoc/c_2810
http://aims.fao.org/aos/agrovoc/c_36669
http://aims.fao.org/aos/agrovoc/c_8504
http://aims.fao.org/aos/agrovoc/c_4852
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_32257
http://aims.fao.org/aos/agrovoc/c_331583
http://aims.fao.org/aos/agrovoc/c_4592
http://aims.fao.org/aos/agrovoc/c_4848
http://aims.fao.org/aos/agrovoc/c_7427
http://aims.fao.org/aos/agrovoc/c_35657
http://aims.fao.org/aos/agrovoc/c_7170
http://aims.fao.org/aos/agrovoc/c_389fe908
http://aims.fao.org/aos/agrovoc/c_4086
F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
fumier
agroécosystème
Zea mays
ressource minérale
carbone
Tithonia
séquestration du carbone
engrais organique
teneur en éléments minéraux
stockage
matière organique du sol
fertilité du sol
carbone organique du sol
http://aims.fao.org/aos/agrovoc/c_2810
http://aims.fao.org/aos/agrovoc/c_36669
http://aims.fao.org/aos/agrovoc/c_8504
http://aims.fao.org/aos/agrovoc/c_4852
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_32257
http://aims.fao.org/aos/agrovoc/c_331583
http://aims.fao.org/aos/agrovoc/c_4592
http://aims.fao.org/aos/agrovoc/c_4848
http://aims.fao.org/aos/agrovoc/c_7427
http://aims.fao.org/aos/agrovoc/c_35657
http://aims.fao.org/aos/agrovoc/c_7170
http://aims.fao.org/aos/agrovoc/c_389fe908
http://aims.fao.org/aos/agrovoc/c_4086
spellingShingle F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
fumier
agroécosystème
Zea mays
ressource minérale
carbone
Tithonia
séquestration du carbone
engrais organique
teneur en éléments minéraux
stockage
matière organique du sol
fertilité du sol
carbone organique du sol
http://aims.fao.org/aos/agrovoc/c_2810
http://aims.fao.org/aos/agrovoc/c_36669
http://aims.fao.org/aos/agrovoc/c_8504
http://aims.fao.org/aos/agrovoc/c_4852
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_32257
http://aims.fao.org/aos/agrovoc/c_331583
http://aims.fao.org/aos/agrovoc/c_4592
http://aims.fao.org/aos/agrovoc/c_4848
http://aims.fao.org/aos/agrovoc/c_7427
http://aims.fao.org/aos/agrovoc/c_35657
http://aims.fao.org/aos/agrovoc/c_7170
http://aims.fao.org/aos/agrovoc/c_389fe908
http://aims.fao.org/aos/agrovoc/c_4086
F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
fumier
agroécosystème
Zea mays
ressource minérale
carbone
Tithonia
séquestration du carbone
engrais organique
teneur en éléments minéraux
stockage
matière organique du sol
fertilité du sol
carbone organique du sol
http://aims.fao.org/aos/agrovoc/c_2810
http://aims.fao.org/aos/agrovoc/c_36669
http://aims.fao.org/aos/agrovoc/c_8504
http://aims.fao.org/aos/agrovoc/c_4852
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_32257
http://aims.fao.org/aos/agrovoc/c_331583
http://aims.fao.org/aos/agrovoc/c_4592
http://aims.fao.org/aos/agrovoc/c_4848
http://aims.fao.org/aos/agrovoc/c_7427
http://aims.fao.org/aos/agrovoc/c_35657
http://aims.fao.org/aos/agrovoc/c_7170
http://aims.fao.org/aos/agrovoc/c_389fe908
http://aims.fao.org/aos/agrovoc/c_4086
Laub, Moritz
Corbeels, Marc
Couedel, Antoine
Ndungu, Samuel Mathu
Mucheru-Muna, Monicah Wanjiku
Mugendi, Daniel
Necpalova, Magdalena
Waswa, Wycliffe
Van de Broek, Marijn
Vanlauwe, Bernard
Six, Johan
Managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in Kenya
description In sub-Saharan Africa, maize is one of the most important staple crops, but long-term maize cropping with low external inputs has been associated with the loss of soil fertility. While adding high-quality organic resources combined with mineral fertilizer has been proposed to counteract this fertility loss, the long-term effectiveness and interactions with site properties still require more understanding. This study used repeated measurements over time to assess the effect of different quantities and qualities of organic resource addition combined with mineral nitrogen (N) on the change of soil organic carbon (SOC) contents over time (and SOC stocks in the year 2021) in four ongoing long-term experiments in Kenya. These experiments were established with identical treatments in moist to dry climates, on coarse to clayey soil textures, and have been conducted for at least 16 years. They received organic resources in quantities equivalent to 1.2 and 4 t C ha−1 yr−1 in the form of Tithonia diversifolia (high quality, fast turnover), Calliandra calothyrsus (high quality, intermediate turnover), Zea mays stover (low quality, fast turnover), sawdust (low quality, slow turnover) and local farmyard manure (variable quality, intermediate turnover). Furthermore, the addition of 240 kg N ha−1 yr−1 as mineral N fertilizer or no fertilizer was the split-plot treatment. At all four sites, a loss of SOC was predominantly observed, likely because the sites had been converted to cropland only a few decades before the start of the experiments. Across sites, the average decline of SOC content over 19 years in the 0 to 15 cm topsoil layer ranged from 42 % to 13 % of the initial SOC content for the control and the farmyard manure treatments at 4 t C ha−1 yr−1, respectively. Adding Calliandra or Tithonia at 4 t C ha−1 yr−1 limited the loss of SOC contents to about 24 % of initial SOC, while the addition of sawdust, maize stover (in three of the four sites) and sole mineral N addition showed no significant reduction of SOC loss over the control. Site-specific analyses, however, did show that at the site with the lowest initial SOC content (about 6 g kg−1), the addition of 4 t C ha−1 yr−1 farmyard manure or Calliandra with mineral N led to a gain in SOC contents. The other sites lost SOC in all treatments, albeit at site-specific rates. While subsoil SOC stocks in 2021 were little affected by organic resource additions (no difference in three of the four sites), the topsoil SOC stocks corroborated the results obtained from the SOC content measurements (0–15 cm) over time. The relative annual change of SOC contents showed a higher site specificity in farmyard manure, Calliandra and Tithonia treatments than in the control treatment, suggesting that the drivers of site specificity in SOC buildup (soil mineralogy, soil texture, climate) need to be better understood for effective targeting management of organic resources. Farmyard manure showed the highest potential for reducing SOC losses, but the necessary quantities to build SOC are often not realistic for smallholder farmers in Africa. Therefore, additional agronomic interventions such as intercropping, crop rotations or the cultivation of crops with extended root systems are necessary to maintain or increase SOC.
format article
topic_facet F08 - Systèmes et modes de culture
P33 - Chimie et physique du sol
fumier
agroécosystème
Zea mays
ressource minérale
carbone
Tithonia
séquestration du carbone
engrais organique
teneur en éléments minéraux
stockage
matière organique du sol
fertilité du sol
carbone organique du sol
http://aims.fao.org/aos/agrovoc/c_2810
http://aims.fao.org/aos/agrovoc/c_36669
http://aims.fao.org/aos/agrovoc/c_8504
http://aims.fao.org/aos/agrovoc/c_4852
http://aims.fao.org/aos/agrovoc/c_1301
http://aims.fao.org/aos/agrovoc/c_32257
http://aims.fao.org/aos/agrovoc/c_331583
http://aims.fao.org/aos/agrovoc/c_4592
http://aims.fao.org/aos/agrovoc/c_4848
http://aims.fao.org/aos/agrovoc/c_7427
http://aims.fao.org/aos/agrovoc/c_35657
http://aims.fao.org/aos/agrovoc/c_7170
http://aims.fao.org/aos/agrovoc/c_389fe908
http://aims.fao.org/aos/agrovoc/c_4086
author Laub, Moritz
Corbeels, Marc
Couedel, Antoine
Ndungu, Samuel Mathu
Mucheru-Muna, Monicah Wanjiku
Mugendi, Daniel
Necpalova, Magdalena
Waswa, Wycliffe
Van de Broek, Marijn
Vanlauwe, Bernard
Six, Johan
author_facet Laub, Moritz
Corbeels, Marc
Couedel, Antoine
Ndungu, Samuel Mathu
Mucheru-Muna, Monicah Wanjiku
Mugendi, Daniel
Necpalova, Magdalena
Waswa, Wycliffe
Van de Broek, Marijn
Vanlauwe, Bernard
Six, Johan
author_sort Laub, Moritz
title Managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in Kenya
title_short Managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in Kenya
title_full Managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in Kenya
title_fullStr Managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in Kenya
title_full_unstemmed Managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in Kenya
title_sort managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in kenya
url http://agritrop.cirad.fr/608540/
http://agritrop.cirad.fr/608540/1/ID608540.pdf
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spelling dig-cirad-fr-6085402024-03-04T15:34:57Z http://agritrop.cirad.fr/608540/ http://agritrop.cirad.fr/608540/ Managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in Kenya. Laub Moritz, Corbeels Marc, Couedel Antoine, Ndungu Samuel Mathu, Mucheru-Muna Monicah Wanjiku, Mugendi Daniel, Necpalova Magdalena, Waswa Wycliffe, Van de Broek Marijn, Vanlauwe Bernard, Six Johan. 2023. Soil, 9 (1) : 301-323.https://doi.org/10.5194/soil-9-301-2023 <https://doi.org/10.5194/soil-9-301-2023> Managing soil organic carbon in tropical agroecosystems: evidence from four long-term experiments in Kenya Laub, Moritz Corbeels, Marc Couedel, Antoine Ndungu, Samuel Mathu Mucheru-Muna, Monicah Wanjiku Mugendi, Daniel Necpalova, Magdalena Waswa, Wycliffe Van de Broek, Marijn Vanlauwe, Bernard Six, Johan eng 2023 Soil F08 - Systèmes et modes de culture P33 - Chimie et physique du sol fumier agroécosystème Zea mays ressource minérale carbone Tithonia séquestration du carbone engrais organique teneur en éléments minéraux stockage matière organique du sol fertilité du sol carbone organique du sol http://aims.fao.org/aos/agrovoc/c_2810 http://aims.fao.org/aos/agrovoc/c_36669 http://aims.fao.org/aos/agrovoc/c_8504 http://aims.fao.org/aos/agrovoc/c_4852 http://aims.fao.org/aos/agrovoc/c_1301 http://aims.fao.org/aos/agrovoc/c_32257 http://aims.fao.org/aos/agrovoc/c_331583 http://aims.fao.org/aos/agrovoc/c_4592 http://aims.fao.org/aos/agrovoc/c_4848 http://aims.fao.org/aos/agrovoc/c_7427 http://aims.fao.org/aos/agrovoc/c_35657 http://aims.fao.org/aos/agrovoc/c_7170 http://aims.fao.org/aos/agrovoc/c_389fe908 Kenya http://aims.fao.org/aos/agrovoc/c_4086 In sub-Saharan Africa, maize is one of the most important staple crops, but long-term maize cropping with low external inputs has been associated with the loss of soil fertility. While adding high-quality organic resources combined with mineral fertilizer has been proposed to counteract this fertility loss, the long-term effectiveness and interactions with site properties still require more understanding. This study used repeated measurements over time to assess the effect of different quantities and qualities of organic resource addition combined with mineral nitrogen (N) on the change of soil organic carbon (SOC) contents over time (and SOC stocks in the year 2021) in four ongoing long-term experiments in Kenya. These experiments were established with identical treatments in moist to dry climates, on coarse to clayey soil textures, and have been conducted for at least 16 years. They received organic resources in quantities equivalent to 1.2 and 4 t C ha−1 yr−1 in the form of Tithonia diversifolia (high quality, fast turnover), Calliandra calothyrsus (high quality, intermediate turnover), Zea mays stover (low quality, fast turnover), sawdust (low quality, slow turnover) and local farmyard manure (variable quality, intermediate turnover). Furthermore, the addition of 240 kg N ha−1 yr−1 as mineral N fertilizer or no fertilizer was the split-plot treatment. At all four sites, a loss of SOC was predominantly observed, likely because the sites had been converted to cropland only a few decades before the start of the experiments. Across sites, the average decline of SOC content over 19 years in the 0 to 15 cm topsoil layer ranged from 42 % to 13 % of the initial SOC content for the control and the farmyard manure treatments at 4 t C ha−1 yr−1, respectively. Adding Calliandra or Tithonia at 4 t C ha−1 yr−1 limited the loss of SOC contents to about 24 % of initial SOC, while the addition of sawdust, maize stover (in three of the four sites) and sole mineral N addition showed no significant reduction of SOC loss over the control. Site-specific analyses, however, did show that at the site with the lowest initial SOC content (about 6 g kg−1), the addition of 4 t C ha−1 yr−1 farmyard manure or Calliandra with mineral N led to a gain in SOC contents. The other sites lost SOC in all treatments, albeit at site-specific rates. While subsoil SOC stocks in 2021 were little affected by organic resource additions (no difference in three of the four sites), the topsoil SOC stocks corroborated the results obtained from the SOC content measurements (0–15 cm) over time. The relative annual change of SOC contents showed a higher site specificity in farmyard manure, Calliandra and Tithonia treatments than in the control treatment, suggesting that the drivers of site specificity in SOC buildup (soil mineralogy, soil texture, climate) need to be better understood for effective targeting management of organic resources. Farmyard manure showed the highest potential for reducing SOC losses, but the necessary quantities to build SOC are often not realistic for smallholder farmers in Africa. Therefore, additional agronomic interventions such as intercropping, crop rotations or the cultivation of crops with extended root systems are necessary to maintain or increase SOC. article info:eu-repo/semantics/article Journal Article info:eu-repo/semantics/publishedVersion http://agritrop.cirad.fr/608540/1/ID608540.pdf text cc_by info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/ https://doi.org/10.5194/soil-9-301-2023 10.5194/soil-9-301-2023 info:eu-repo/semantics/altIdentifier/doi/10.5194/soil-9-301-2023 info:eu-repo/semantics/altIdentifier/purl/https://doi.org/10.5194/soil-9-301-2023 info:eu-repo/grantAgreement/EC/H2020/ANR-10-LABX-0001//(FRA) Agricultural Sciences for sustainable Development/AGRO info:eu-repo/grantAgreement/EC/H2020/172940//(CHE) Agricultural Intensification and Dynamics of Soil Carbon Sequestration in Tropical and Temperate Farming Systems/DSCATT info:eu-repo/grantAgreement/EC/H2020/869367//(EU) Land Use Based Mitigation for Resilient Climate Pathways/LANDMARC