Tree biomass and soil organic carbon densities across the Sudanese woodland savannah: A regional carbon sequestration study
Mean tree biomass and soil carbon (C) densities for 39 map sheet grids (1° lat. × 1.5° long.) covering the Acacia woodland savannah region of Sudan (10–16° N; 21–36° E) are presented. Data from the National Forest Inventory of Sudan, Harmonized World Soil Database and FAO Local Climate Estimator wer...
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Published in | Journal of arid environments Vol. 89; pp. 67 - 76 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Kidlington
Elsevier Ltd
01.02.2013
Elsevier |
Subjects | |
Online Access | Get full text |
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Summary: | Mean tree biomass and soil carbon (C) densities for 39 map sheet grids (1° lat. × 1.5° long.) covering the Acacia woodland savannah region of Sudan (10–16° N; 21–36° E) are presented. Data from the National Forest Inventory of Sudan, Harmonized World Soil Database and FAO Local Climate Estimator were used to calculate C densities, mean annual precipitation (MAP) and mean annual temperature (MAT). Above-ground biomass C and soil organic carbon (SOC, 1 m) densities averaged 112 and 5453 g C m−2, respectively. Below-ground biomass C densities, estimated using root shoot ratios, averaged 33 g C m−2. Biomass C densities and MAP increased southwards across the region while SOC densities were lowest in the centre of the region and increased westwards and eastwards. Both above-ground biomass C and SOC densities were significantly (p < 0.05) correlated with MAP (rs = 0.84 and rs = 0.34, respectively) but showed non-significant correlations with MAT (rs = −0.22 and rs = 0.24, respectively). SOC densities were significantly correlated with biomass C densities (rs = 0.34). The results indicated substantial under stocking of trees and depletion of SOC, and potential for C sequestration. Up-to-date regional and integrated soil and forest inventories are required for planning improved land-use management and restoration.
► Sudanese woodland savannah tree biomass C and SOC (1 m) densities were estimated. ► Above-ground biomass C and SOC densities averaged 112 and 5453 g C m−2. ► SOC densities significantly correlated with above-ground biomass C densities. ► Biomass C and SOC densities significantly correlated with MAP, but not with MAT. ► C densities across the region are considerably below sequestration potential. |
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Bibliography: | http://dx.doi.org/10.1016/j.jaridenv.2012.10.002 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0140-1963 1095-922X |
DOI: | 10.1016/j.jaridenv.2012.10.002 |