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The impact of land use and land cover (LULC) dynamics on soil erosion and sediment yield in Ethiopia

机译:土地利用和土地覆被(LULC)动态对埃塞俄比亚土壤侵蚀和沉积物产量的影响

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摘要

The central highlands of Ethiopia are characterized as a region of high rates of land degradation and soil erosion. This study aimed to estimate total amount of soil loss and sediment yield using RUSLE model within GIS environment. LULC maps of 1973–2015 were used to evaluate the impact of land use change on soil loss and sediment yield. Each model parameter and sediment deliver ration was computed by using Williams and Berndt empirical equation. The net soil erosion and sediment yield at the Guder river mouth and soil risk map was estimated for the watershed. LULC dynamic for the study period and watershed have shown that there existed a rapid conversion of vegetated land uses to human modified land uses. The study revealed that the mean soil loss from the watershed ranges between 25 and 30 t/ha−1 yr−1 which accounted 25.8, 28.7 and 30.3 t/ha/yr for 1973, 1995 and 2015 periods respectively. The estimated total soil loss in 1973, 1995 and 2015 periods were 198Mt yr-1, 221Mt yr-1 and 239Mt yr-1 respectively. The mean sediment yield estimated was 6.79, 8.65 and 9.44t ha-1 yr-1 for 1973, 1995 and 2015 periods respectively. The sediment deliver ratio (SDR) of the watershed ranged between 0 and 0.26. The spatial distribution of SDR showed that the highest value was recorded on central and eastern part of the watershed. Prioritizing erosion host spot areas is recommended to rehabilitate degraded lands using suitable soil and water conservation structures.
机译:埃塞俄比亚中部高地的特点是土地退化和水土流失率很高。这项研究旨在使用GIS环境中的RUSLE模型估算土壤流失和沉积物产量的总量。 1973-2015年的LULC地图用于评估土地利用变化对土壤流失和沉积物产量的影响。使用Williams和Berndt经验方程式计算每个模型参数和沉积物的定量比。对该流域估算了古德河口和土壤风险图的土壤净侵蚀和沉积物产量。研究期和分水岭的土地利用,土地利用变化和林业动态表明,植被土地利用已迅速转变为人类改良土地利用。研究表明,该流域的平均土壤流失范围为25至30 t / ha-1 yr-1,分别在1973年,1995年和2015年分别为25.8、28.7和30.3 t / ha / yr。估计1973年,1995年和2015年的土壤流失总量分别为198Mt yr-1、221Mt yr-1和239Mt yr-1。 1973年,1995年和2015年的平均沉积物产量估计分别为6.79、8.65和9.44t ha-1 yr-1。流域的沉积物输送比(SDR)介于0和0.26之间。 SDR的空间分布表明最高值记录在流域的中部和东部。建议优先考虑侵蚀宿主点区域,以使用合适的水土保持结构修复退化土地。

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