Kidane Moges, Bezie Alemu, Kesete Nega, Tolessa Terefe
College of Agriculture and Veterinary Sciences, Ambo University, Ethiopia.
Institute of Cooperatives and Development Studies, Ambo University, Ethiopia.
Heliyon. 2019 Dec 16;5(12):e02981. doi: 10.1016/j.heliyon.2019.e02981. eCollection 2019 Dec.
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.
埃塞俄比亚的中部高地被视为土地退化和土壤侵蚀率较高的地区。本研究旨在利用地理信息系统(GIS)环境下的通用土壤流失方程(RUSLE)模型估算土壤流失总量和产沙量。使用1973 - 2015年的土地利用/土地覆盖(LULC)地图来评估土地利用变化对土壤流失和产沙量的影响。每个模型参数和泥沙输送比通过威廉姆斯和伯恩特经验方程计算得出。估算了古德河口的净土壤侵蚀量、产沙量以及该流域的土壤风险图。研究期间该流域的LULC动态变化表明,植被覆盖的土地利用类型迅速转变为人类改造的土地利用类型。研究表明,该流域的平均土壤流失量在25至30吨/公顷·年之间,1973年、1995年和2015年分别为25.8吨/公顷/年、28.7吨/公顷/年和30.3吨/公顷/年。1973年、1995年和2015年估算的土壤流失总量分别为19800万吨/年、22100万吨/年和23900万吨/年。1973年、1995年和2015年估算的平均产沙量分别为6.79吨/公顷·年、8.65吨/公顷·年和9.44吨/公顷·年。该流域的泥沙输送比(SDR)在0至0.26之间。SDR的空间分布表明,该流域中部和东部记录到的数值最高。建议优先确定侵蚀热点地区,以便使用合适的水土保持结构对退化土地进行恢复治理。