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Comprehensive assessment of soil erosion risk for better land use planning in river basins : case study of the Upper Blue Nile River

机译:综合评价土壤侵蚀风险,改善流域土地利用规划 - 以上青尼罗河为例

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摘要

In the drought-prone Upper Blue Nile River (UBNR) basin of Ethiopia, soil erosion by water results in significant consequences that also affect downstream countries. However, there have been limited comprehensive studies of this and other basins with diverse agroecologies. We analyzed the variability of gross soil loss and sediment yield rates under present and expected future conditions using a newly devised methodological framework. The results showed that the basin generates an average soil loss rate of 27.5 t ha(-1) yr(-1) and a gross soil loss of ca. 473 Mt yr(-1), of which, at least 10% comes from gully erosion and 26.7% leaves Ethiopia. In a factor analysis, variation in agroecology (average factor score = 1.32) and slope (1.28) were the two factors most responsible for this high spatial variability. About 39% of the basin area is experiencing severe to very severe (>30 t ha(-1) yr(-1)) soil erosion risk, which is strongly linked to population density. Severe or very severe soil erosion affects the largest proportion of land in three subbasins of the UBNR basin: Blue Nile 4 (53.9%), Blue Nile 3 (45.1%), and Jema Shet (42.5%). If appropriate soil and water conservation practices targeted ca. 77.3% of the area with moderate to severe erosion (>15 t ha(-1) yr(-1)), the total soil loss from the basin could be reduced by ca. 52%. Our methodological framework identified the potential risk for soil erosion in large-scale zones, and with a more sophisticated model and input data of higher spatial and temporal resolution, results could be specified locally within these risk zones. Accurate assessment of soil erosion in the UBNR basin would support sustainable use of the basin's land resources and possibly open up prospects for cooperation in the Eastern Nile region.
机译:在容易干旱的埃塞俄比亚上尼罗河上游流域,水土流失造成了严重后果,也影响了下游国家。但是,对该流域和其他流域具有不同农业生态的综合研究很少。我们使用一种新设计的方法框架,分析了当前和未来预期条件下的总土壤流失和沉积物产率的变化。结果表明,该盆地的平均土壤流失率为27.5 t ha(-1)yr(-1),总土壤流失率为ca。 473 Mt yr(-1),其中至少10%来自沟壑侵蚀,而26.7%离开埃塞俄比亚。在因子分析中,农业生态的变化(平均因子得分= 1.32)和斜率(1.28)是造成这种高空间变异性的两个主要原因。流域面积约39%面临着严重到非常严重(> 30 t ha(-1)yr(-1)的土壤侵蚀风险,这与人口密度密切相关。严重或非常严重的水土流失影响了UBNR盆地三个子盆地中最大比例的土地:青尼罗河4(53.9%),青尼罗河3(45.1%)和杰玛·谢特(42.5%)。如果合适,水土保持措施的目标是ca。在中度至重度侵蚀(> 15 t ha(-1)yr(-1))面积的77.3%下,流域的总土壤流失量可减少约。 52%。我们的方法框架确定了大规模地区水土流失的潜在风险,并且通过更复杂的模型和更高时空分辨率的输入数据,可以在这些风险区内局部指定结果。准确评估UBNR流域的土壤侵蚀将支持流域土地资源的可持续利用,并可能为尼罗河东部地区的合作开辟前景。

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