首页> 外文期刊>Journal of Remote Sensing & GIS >GIS-RUSLE Interphase Modelling of Soil Erosion Hazard and Estimation of Sediment Yield for River Nzoia Basin in Kenya
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GIS-RUSLE Interphase Modelling of Soil Erosion Hazard and Estimation of Sediment Yield for River Nzoia Basin in Kenya

机译:肯尼亚恩佐亚河流域土壤侵蚀危险性的GIS-RUSLE相变模型及产沙量估算。

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River Nzoia basin is predisposed to degradation attributed to poor anthropogenic land use practices, soil erosion and sedimentation. The objective of this study was to model soil erosion hazard and estimate sediment yield for river Nzoia basin. Database of the basin comprised of 90 m DEM, LandSat imagery, rainfall, and soil data. Simulated RUSLE model factors (R, K, LS, and C) were multiplied using the raster calculator in ArcGIS 10.1. This generated the soil erosion hazard map for river Nzoia basin with an average annual soil loss rate of 0.51 and a maximum of 8.84 Mton ha-1 yr-1. This translates into a mean annual soil loss of 6.579 × 105 Mtonyr-1. Sediment Delivery Ratio (SDR) of 0.121 revealed that 87.9% of the soil eroded by water in the basin is deposited before reaching the basin outlet. Average annual sediment yield estimated was 0.06 Mtonyr-1. Soil erosion modeling results showed that river Nzoia basin is experiencing varying erosion rates spatially. The interplay among the RUSLE factors strongly influence average annual soil loss rates. Areas experiencing high soil loss rates are closely linked to annual cropland, deforested and high elevation points. Low rates of soil loss are attributable to soil conservation practices and protected areas such as game parks. Thus, there is a close coupling between soil loss and land use category in river Nzoia basin. Sustainable land use practices should be embraced to support conservation programmes to mitigate soil erosion, prevent sedimentation and reduce sediment yield in the river channel.
机译:恩佐亚河流域由于人为的土地使用方式不佳,土壤侵蚀和沉积而易于退化。这项研究的目的是为Nzoia流域的水土流失危害建模并估算沉积物产量。流域数据库包括90 m DEM,LandSat影像,降雨量和土壤数据。使用ArcGIS 10.1中的栅格计算器将模拟的RUSLE模型因子(R,K,LS和C)相乘。这产生了恩佐亚河流域的水土流失危害图,年平均土壤流失率为0.51,最大值为8.84 Mton ha-1 yr-1。这意味着年平均土壤流失量为6.579×105 Mtonyr-1。沉积物输送比(SDR)为0.121,表明流域内水侵蚀的土壤中87.9%在到达流域出水口之前已经沉积。估计的年平均沉积物产量为0.06 Mtonyr-1。水土流失模拟结果表明,恩佐亚河流域的空间侵蚀速率在变化。 RUSLE因子之间的相互作用强烈影响年平均土壤流失率。土壤流失率高的地区与一年生农田,森林砍伐和高海拔地区密切相关。土壤流失率低归因于土壤保护做法和保护区,例如游戏公园。因此,恩佐亚河流域的土壤流失与土地利用类别之间有着密切的联系。应采纳可持续的土地利用方式,以支持保护计划,以减轻水土流失,防止沉积和减少河道中的沉积物产量。

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