Soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in South African savannas

Woody plant encroachment has transformed land-cover patterns in savannas and grasslands throughout the world, with implications for changes in soil organic carbon (SOC) dynamics. However, our understanding of the effects of woody encroachment on SOC is very limited. In a study of pairs of neighbouri...

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Main Authors: Mureva, Admore, Chivenge, Pauline, Ward, David
Format: Journal Article
Language:Inglés
Published: Commonwealth Scientific and Industrial Research Organisation 2021
Subjects:
Online Access:https://hdl.handle.net/10568/164310
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author Mureva, Admore
Chivenge, Pauline
Ward, David
author_browse Chivenge, Pauline
Mureva, Admore
Ward, David
author_facet Mureva, Admore
Chivenge, Pauline
Ward, David
author_sort Mureva, Admore
collection Repository of Agricultural Research Outputs (CGSpace)
description Woody plant encroachment has transformed land-cover patterns in savannas and grasslands throughout the world, with implications for changes in soil organic carbon (SOC) dynamics. However, our understanding of the effects of woody encroachment on SOC is very limited. In a study of pairs of neighbouring, woody encroached and grassland plots along a rainfall gradient (300–1500 mm mean annual precipitation, MAP) in South African savannas, we quantified the changes in SOC and nitrogen pools to a depth of 100 cm, in three soil physical fractions (coarse particulate organic matter, macroaggregates and silt and clay) and bulk soil. The 0–10 cm soil layer of the 1500 mm MAP site lost 26% of SOC stocks due to shrub encroachment. Contrastingly, the 300 and 350 mm MAP sites gained 24% and 27% total SOC, respectively, due to shrub encroachment. In the soil fractions, the largest changes in SOC, ranging within 2.64–464%, were in the coarse particulate organic matter (unprotected organic matter > 250 μm), and the lowest in the silt and clay fraction (6–32%) across all sites and depths. Soil nitrogen increased across all encroached sites compared with open grasslands, regardless of MAP. For every 1-unit increase in MAP and soil fraction size there was a change of –0.06 and 0.1 SOC (gC/kg soil) in encroached grasslands, respectively. We conclude that shrub-encroached grasslands potentially sequester more C in soils of arid regions than in humid regions. At three of our sites, we were unable to differentiate SOC between encroached and open-grassland soils from bulk soil but could do so from soil fraction analysis. Thus, soil fraction analysis is a more effective way to assess changes in soil C than bulk soil.
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spelling CGSpace1643102025-12-08T10:29:22Z Soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in South African savannas Mureva, Admore Chivenge, Pauline Ward, David earth-surface processes soil science environmental science (miscellaneous) Woody plant encroachment has transformed land-cover patterns in savannas and grasslands throughout the world, with implications for changes in soil organic carbon (SOC) dynamics. However, our understanding of the effects of woody encroachment on SOC is very limited. In a study of pairs of neighbouring, woody encroached and grassland plots along a rainfall gradient (300–1500 mm mean annual precipitation, MAP) in South African savannas, we quantified the changes in SOC and nitrogen pools to a depth of 100 cm, in three soil physical fractions (coarse particulate organic matter, macroaggregates and silt and clay) and bulk soil. The 0–10 cm soil layer of the 1500 mm MAP site lost 26% of SOC stocks due to shrub encroachment. Contrastingly, the 300 and 350 mm MAP sites gained 24% and 27% total SOC, respectively, due to shrub encroachment. In the soil fractions, the largest changes in SOC, ranging within 2.64–464%, were in the coarse particulate organic matter (unprotected organic matter > 250 μm), and the lowest in the silt and clay fraction (6–32%) across all sites and depths. Soil nitrogen increased across all encroached sites compared with open grasslands, regardless of MAP. For every 1-unit increase in MAP and soil fraction size there was a change of –0.06 and 0.1 SOC (gC/kg soil) in encroached grasslands, respectively. We conclude that shrub-encroached grasslands potentially sequester more C in soils of arid regions than in humid regions. At three of our sites, we were unable to differentiate SOC between encroached and open-grassland soils from bulk soil but could do so from soil fraction analysis. Thus, soil fraction analysis is a more effective way to assess changes in soil C than bulk soil. 2021-03-18 2024-12-19T12:53:44Z 2024-12-19T12:53:44Z Journal Article https://hdl.handle.net/10568/164310 en Commonwealth Scientific and Industrial Research Organisation Mureva, Admore; Chivenge, Pauline and Ward, David. 2021. Soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in South African savannas. Soil Res., Volume 59 no. 6 p. 595-608
spellingShingle earth-surface processes
soil science
environmental science (miscellaneous)
Mureva, Admore
Chivenge, Pauline
Ward, David
Soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in South African savannas
title Soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in South African savannas
title_full Soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in South African savannas
title_fullStr Soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in South African savannas
title_full_unstemmed Soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in South African savannas
title_short Soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in South African savannas
title_sort soil organic carbon and nitrogen in soil physical fractions in woody encroached grassland in south african savannas
topic earth-surface processes
soil science
environmental science (miscellaneous)
url https://hdl.handle.net/10568/164310
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AT warddavid soilorganiccarbonandnitrogeninsoilphysicalfractionsinwoodyencroachedgrasslandinsouthafricansavannas