Estimating soil erosion in sub-Saharan Africa based on landscape similarity mapping and using the revised universal soil loss equation (RUSLE)

被引:0
作者
Lulseged Tamene
Quang Bao Le
机构
[1] Chitedze Agricultural Research Station,International Center for Tropical Agriculture (CIAT)
[2] Swiss Federal Institute of Technology Zurich (ETH Zurich),Department of Environmental Systems Science
[3] CGIAR Research Program on Dryland Systems,undefined
[4] C/o International Center for Agricultural Research in Dry Areas (ICARDA),undefined
来源
Nutrient Cycling in Agroecosystems | 2015年 / 102卷
关键词
Soil erosion; Erosion modeling; Landscape similarity; RUSLE; White Volta Basin; Nile Basin; Sub-Saharan Africa;
D O I
暂无
中图分类号
学科分类号
摘要
Soil erosion is one of the major forms of land degradation in sub-Saharan Africa (SSA) with serious impact on agricultural productivity. Due to the absence of reliable data at appropriate resolution and differences in the methods used, there are discrepancies in soil erosion estimates at both continental and basin levels. This study attempts to contribute to the existing regional soil erosion estimates based on a two-stage approach. First, we partitioned SSA into environmental units, so-called similar environmental constraint envelops (SECEs), using broad scale data as proxies of erosion drivers. The SECEs are intended to provide spatial frame for scaling out modeled erosion results. Second, soil erosion estimate is made at two selected basins of the White Volta and the Nile using spatially distributed revised universal soil loss (RUSLE) model. The delineation of SECEs across SSA provided spatially differentiated clusters governed by the existence of similar environmental conditions and soil erosion risk levels. The RUSLE-based estimates show that soil erosion ranges between 0 to 120 t ha−1 yr−1 (overall mean of 35 t ha−1 yr−1) in the White Volta basin, and 0–650 t ha−1 yr−1 (overall mean of 75 t ha−1 yr−1) in the Nile basin. The soil loss estimates show an overall agreement with other studies conducted in the two basins. Our approach provides guidance on where empirically estimated soil erosion for a given SECE can be extrapolated to similar SECE’s with acceptable confidence and where finer SECE’s sub-units should be defined to further collapse the spatial variability of drivers of erosion.
引用
收藏
页码:17 / 31
页数:14
相关论文
共 135 条
[1]  
Abe SS(2011)Sawah ecotechnology—a trigger for a rice green revolution in sub-Saharan Africa: basic concept and policy implications Outlook Agric 40 221-227
[2]  
Wakatsuki T(2009)Assessing sediment inputs to small reservoirs in Upper East Region, Ghana Lakes Reserv Res Manag 14 279-287
[3]  
Adwubi A(2001)Options for increasing carbon sequestration in West African soils: an explanatory study with special focus on Senegal Land Degrad Dev 12 131-142
[4]  
Amegashie BK(2011)Sediment management modelling in the Blue Nile basin using SWAT model Hydrol Earth Syst Sci 15 807-818
[5]  
Agyare WA(2003)Predicting hydrologically similar surfaces (HYSS) in semi-arid environments Adv Monit Model 1 1-26
[6]  
Tamene L(2013)Multi-criteria decision making approach for watershed prioritization using analytic hierarchy process technique and GIS Water Resour Manag 27 3555-3571
[7]  
Odai SN(2004)Guidelines for reporting statistics in journals published by the American Physiological Society Adv Physiol Educ 28 85-87
[8]  
Quansah C(2010)African green revolution needn’t be a mirage Science 327 831-832
[9]  
Vlek PLG(1997)Identification of critical sediment source areas at regional level Phys Chem Earth 22 355-359
[10]  
Batjes NH(1996)Hydrological Response Units (HRUs) as modelling entities for hydrological river basin simulation and their methodological potential for modelling complex environment process systems. Results from the Sieg Catchment Erde 127 43-62