Soil organic carbon and related properties under conservation agriculture and contrasting conventional fields in Northern Malawi

Conservation agriculture (CA) is widely promoted as an agroecology-based approach for soil conservation. Several studies have focused on effects of CA on crop yields and soil moisture dynamics in sub-Saharan Africa, with limited focus on effects of CA on soil organic carbon (SOC) and associated frac...

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Main Authors: Muneta G. Manzeke-Kangara, Ivy S. Ligowe, Austin Tibu, Timothy N. Gondwe, Henry M. R. Greathead, Marcelo V. Galdos
Format: Article
Language:English
Published: Frontiers Media S.A. 2025-02-01
Series:Frontiers in Soil Science
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Online Access:https://www.frontiersin.org/articles/10.3389/fsoil.2024.1481275/full
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author Muneta G. Manzeke-Kangara
Ivy S. Ligowe
Austin Tibu
Timothy N. Gondwe
Henry M. R. Greathead
Marcelo V. Galdos
Marcelo V. Galdos
author_facet Muneta G. Manzeke-Kangara
Ivy S. Ligowe
Austin Tibu
Timothy N. Gondwe
Henry M. R. Greathead
Marcelo V. Galdos
Marcelo V. Galdos
author_sort Muneta G. Manzeke-Kangara
collection DOAJ
description Conservation agriculture (CA) is widely promoted as an agroecology-based approach for soil conservation. Several studies have focused on effects of CA on crop yields and soil moisture dynamics in sub-Saharan Africa, with limited focus on effects of CA on soil organic carbon (SOC) and associated fractions. We collected representative soil samples from 30 paired farms under CA and conventional tillage in Mzimba district, north of Malawi to determine effects of tillage and soil depth on soil physico-chemical properties, total SOC, and organic carbon fractions. Undisturbed soil cores were collected for bulk density measurements. Different SOC pools were determined using the soil fractionation method, while soil physico-chemical analyses were conducted using standard laboratory methods on disturbed soil samples. Soil organic carbon content ranged from 0.4-1.8% in CA plots. This was significantly larger than SOC contents of 0.4-1.5% measured under conventional tilled plots. Tillage type and soil depth had significant interaction effects on SOC. For example, larger contents of SOC were measured at depths of 0-10 cm compared to 10-30 cm under CA plots. Soil depth had significant effects on most soil properties compared to tillage. Examples include Heavy Particulate Organic Matter-Carbon (POM-C) fraction, Mineral Associated Organic Matter-Carbon (MAOM-C), nitrogen in MAOM fraction and nitrogen in the Light POM fractions. These were larger in the 0-10 cm soil depth than in the 10-30 cm soil depth. In contrast, tillage type only had significant effects on the Heavy POM-C and MAOM-C fractions, which were larger under CA than conventional tilled plots. Conservation agriculture showed capacity to improve total SOC and its associated fractions, a finding relevant towards understanding effects of land management on carbon storage. However, challenges of competing residue use as feed, mulch, and fuel continue to impede mulching under CA systems. Longer term studies and use of alternative mulching options could be employed to recognise noticeable changes in other SOC beneficial pools in fields under CA.
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spelling doaj-art-5eb1ad05a62d4ed2810629ce39ba66e12025-02-04T10:40:18ZengFrontiers Media S.A.Frontiers in Soil Science2673-86192025-02-01410.3389/fsoil.2024.14812751481275Soil organic carbon and related properties under conservation agriculture and contrasting conventional fields in Northern MalawiMuneta G. Manzeke-Kangara0Ivy S. Ligowe1Austin Tibu2Timothy N. Gondwe3Henry M. R. Greathead4Marcelo V. Galdos5Marcelo V. Galdos6Department of Sustainable Soils and Crops, Rothamsted Research, Harpenden, United KingdomDepartment of Forestry and Environmental Management, Mzuzu University, Mzuzu, MalawiEnvironment and Natural Resources Management Department, Lilongwe University of Agriculture and Natural Resources, Lilongwe, MalawiAnimal Science Department, Lilongwe University of Agriculture and Natural Resources, Lilongwe, MalawiSchool of Biology, University of Leeds, Leeds, United KingdomDepartment of Sustainable Soils and Crops, Rothamsted Research, Harpenden, United KingdomSchool of Earth and Environment, University of Leeds, Leeds, United KingdomConservation agriculture (CA) is widely promoted as an agroecology-based approach for soil conservation. Several studies have focused on effects of CA on crop yields and soil moisture dynamics in sub-Saharan Africa, with limited focus on effects of CA on soil organic carbon (SOC) and associated fractions. We collected representative soil samples from 30 paired farms under CA and conventional tillage in Mzimba district, north of Malawi to determine effects of tillage and soil depth on soil physico-chemical properties, total SOC, and organic carbon fractions. Undisturbed soil cores were collected for bulk density measurements. Different SOC pools were determined using the soil fractionation method, while soil physico-chemical analyses were conducted using standard laboratory methods on disturbed soil samples. Soil organic carbon content ranged from 0.4-1.8% in CA plots. This was significantly larger than SOC contents of 0.4-1.5% measured under conventional tilled plots. Tillage type and soil depth had significant interaction effects on SOC. For example, larger contents of SOC were measured at depths of 0-10 cm compared to 10-30 cm under CA plots. Soil depth had significant effects on most soil properties compared to tillage. Examples include Heavy Particulate Organic Matter-Carbon (POM-C) fraction, Mineral Associated Organic Matter-Carbon (MAOM-C), nitrogen in MAOM fraction and nitrogen in the Light POM fractions. These were larger in the 0-10 cm soil depth than in the 10-30 cm soil depth. In contrast, tillage type only had significant effects on the Heavy POM-C and MAOM-C fractions, which were larger under CA than conventional tilled plots. Conservation agriculture showed capacity to improve total SOC and its associated fractions, a finding relevant towards understanding effects of land management on carbon storage. However, challenges of competing residue use as feed, mulch, and fuel continue to impede mulching under CA systems. Longer term studies and use of alternative mulching options could be employed to recognise noticeable changes in other SOC beneficial pools in fields under CA.https://www.frontiersin.org/articles/10.3389/fsoil.2024.1481275/fullbulk densityclimate change mitigationclimate-smart agricultureHeavy Particulate Organic Matter-CarbonLight Particulate Organic Matter-CarbonMineral Associated Organic Matter-Carbon
spellingShingle Muneta G. Manzeke-Kangara
Ivy S. Ligowe
Austin Tibu
Timothy N. Gondwe
Henry M. R. Greathead
Marcelo V. Galdos
Marcelo V. Galdos
Soil organic carbon and related properties under conservation agriculture and contrasting conventional fields in Northern Malawi
Frontiers in Soil Science
bulk density
climate change mitigation
climate-smart agriculture
Heavy Particulate Organic Matter-Carbon
Light Particulate Organic Matter-Carbon
Mineral Associated Organic Matter-Carbon
title Soil organic carbon and related properties under conservation agriculture and contrasting conventional fields in Northern Malawi
title_full Soil organic carbon and related properties under conservation agriculture and contrasting conventional fields in Northern Malawi
title_fullStr Soil organic carbon and related properties under conservation agriculture and contrasting conventional fields in Northern Malawi
title_full_unstemmed Soil organic carbon and related properties under conservation agriculture and contrasting conventional fields in Northern Malawi
title_short Soil organic carbon and related properties under conservation agriculture and contrasting conventional fields in Northern Malawi
title_sort soil organic carbon and related properties under conservation agriculture and contrasting conventional fields in northern malawi
topic bulk density
climate change mitigation
climate-smart agriculture
Heavy Particulate Organic Matter-Carbon
Light Particulate Organic Matter-Carbon
Mineral Associated Organic Matter-Carbon
url https://www.frontiersin.org/articles/10.3389/fsoil.2024.1481275/full
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