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利用 GIS 和 RS 集成的 RUSLE 模型评估土壤侵蚀程度:以埃塞俄比亚西北部 Megech-Dirma 流域为例。

Assessment of soil erosion extent using RUSLE model integrated with GIS and RS: the case of Megech-Dirma watershed, Northwest Ethiopia.

机构信息

Geoinformatics Program, Department of Marine Geology, Mangalore University, Mangalagangothri, Mangalore, 574 199, India.

Geography and Environmental Studies Department, Debre Tabor University, Debra Tabor, Ethiopia.

出版信息

Environ Monit Assess. 2022 Mar 31;194(4):318. doi: 10.1007/s10661-022-09965-y.

Abstract

Soil erosion valuation at a spatial scale is crucial for assessing natural resource quality in a farming country like Ethiopia. The study's goal was to determine the rate of soil erosion in the Megech-Dirma catchment in Northwest Ethiopia using the Revised Universal Soil Loss Equation model aggregation with Geographic Information System and Remote Sensing. Sediment yield and transport were also estimated using sediment delivery ratio. Revised Universal Soil Loss Equation model data inputs included precipitation data for the R value, soil data for the K value, land cover data from satellite images for the C and P value, and topographical data from a Digital Elevation Model for the LS component. It was completed using the ArcGIS 10.4 software. The mean annual soil loss is 110.60 t ha yr. Each year, a total of 8499.74 t ha yr of soil eroded and on average resulting in 1605.30 t/km/yr, sediment material has been transported to the stream channels and deposited with a sediment delivery ratio of 1.87. The strength of soil erosion in the area is divided into six categories. The erosion rate classes were 46.38 percent (0-12 t ha yr) low, 13.63 percent (12-20 ha yr) moderate, 9.22 percent (20-35 ha yr) high, 12.30 percent (35-50 ha yr) very high, 7.20 percent (50 up to 100 ha yr) severe, and 11.27 percent (>100 ha yr) very severe erosion. According to erosion severity, 46.38 percent of the watershed is at risk of low erosion, while 11.27 percent is at risk of extremely severe erosion. The north and northeastern sections of the watershed have a moderate to extremely severe erosion risk due to steep slopes, high rainfall, and weak conservation measures. The severely eroded parts of the plateau and steep portions are proposed to be covered by plantation, stone bund, and check dam constructions.

摘要

在像埃塞俄比亚这样的农业国家,在空间尺度上评估土壤侵蚀对于评估自然资源质量至关重要。本研究的目的是使用修正的通用土壤流失方程模型聚合地理信息系统和遥感技术,确定埃塞俄比亚西北部 Megech-Dirma 集水区的土壤侵蚀速率。还使用泥沙输送比估算了泥沙产量和输移。修正的通用土壤流失方程模型数据输入包括 R 值的降水数据、K 值的土壤数据、C 和 P 值的卫星图像土地覆盖数据以及 LS 分量的数字高程模型地形数据。该研究使用 ArcGIS 10.4 软件完成。平均年土壤流失量为 110.60 t ha-yr。每年,共有 8499.74 t ha-yr的土壤被侵蚀,平均每年每公里有 1605.30 t/km-yr 的泥沙物质被输送到河道并沉积,泥沙输送比为 1.87。该地区土壤侵蚀的强度分为六类。侵蚀速率类别为 46.38%(0-12 t ha-yr)为低,13.63%(12-20 t ha-yr)为中,9.22%(20-35 t ha-yr)为高,12.30%(35-50 t ha-yr)为极高,7.20%(50-100 t ha-yr)为严重,11.27%(>100 t ha-yr)为极严重侵蚀。根据侵蚀严重程度,46.38%的流域面临低侵蚀风险,而 11.27%的流域面临极严重侵蚀风险。流域的北部和东北部由于坡度陡峭、降雨量高和保护措施薄弱,存在中等到极严重的侵蚀风险。高原严重侵蚀区和陡峭区建议采用造林、石堤和挡水坝建设。

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