利用USLE/GIS方法评估埃塞俄比亚青尼罗盆地低地农业流域土壤侵蚀风险高的地区

K. Tsegaye, H. Addis, Ebrahim Esa Hassen
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引用次数: 13

摘要

流域侵蚀图提供了丰富的知识,对于实施特定地点的管理干预措施至关重要。因此,基于流域的土壤侵蚀评价识别侵蚀热点区域,同时利用USLE/GIS方法粗略计算位于埃塞俄比亚青尼罗盆地西北低地的Genda-wuha流域的年平均土壤流失量。Genda-wuha流域总面积为154,548.5 ha。利用16年的降雨数据、53个土壤样本数据、30m × 30m的数字高程模型(DEM)、土地利用/土地覆盖图以及支持实践因子来确定高侵蚀风险区域。利用ArcGIS平台中的栅格计算器对USLE参数进行综合分析,预测和绘制了根大-乌哈流域年平均土壤流失量。结果表明,流域年土壤流失量从中下游的零到陡峭部分的75.36 Mg ha- 1year -1,平均年土壤流失量为7.9 Mg ha- 1year -1。大部分土壤侵蚀影响区在空间上位于根大-乌哈流域的上陡坡区,这可能是由于特定位置的坡度和长度增加所致。然而,大多数流域(82.62%)的侵蚀速率较低,在0 ~ 5 Mg ha-1 - 1 - 1之间,这些地区主要对应于流域的近平坦景观。
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Soil Erosion Impact Assessment using USLE/GIS Approaches to Identify High Erosion Risk Areas in the Lowland Agricultural Watershed of Blue Nile Basin, Ethiopia
Erosion map of a watershed offers a wealth of knowledge and can be crucial for implementing site-specific management interventions. Thus, watershed-based soil erosion assessment was conducted to recognize erosion hotspot areas, while aiming to roughly calculate the average annual soil loss in Genda-wuha watershed, with a total area of 154,548.5 ha located in the northwest lowland of Blue Nile basin Ethiopia using USLE/GIS approach. Sixteen years of rainfall data, 53 soil sample data, a 30m by 30m digital elevation model (DEM), a land-use/land-cover map, and support practice factor were used to determine high erosion risk areas. The USLE parameters were integrated and analyzed using a raster calculator in the ArcGIS platform to predict and map the mean annual soil loss of Genda-wuha watershed. The result showed that the annual soil loss of the watershed extends from none in the lower and middle part of the watershed to 75.36 Megagram (Mg) ha-1yr-1 in the steeper parts of the watershed with a mean annual soil loss of 7.9 Mg ha-1yr-1. Most of the soil erosion affected areas are spatially situated in the upper steep slope parts of Genda-wuha watershed, which could be as a result of an increased slope gradient and length in the specified location. However, the majority of the watershed (82.62%) was estimated to be low erosion rates varying from 0 to 5 Mg ha–1 yr–1 and these areas correspond primarily to nearly flat landscapes of the watershed.
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