GIS-RUSLE Interphase Modelling of Soil Erosion Hazard and Estimation of Sediment Yield for River Nzoia Basin in Kenya

Akali Ngaywa Moses
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引用次数: 15

Abstract

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.
肯尼亚Nzoia河流域土壤侵蚀危害GIS-RUSLE间期模型及产沙量估算
由于不良的人为土地利用做法、土壤侵蚀和沉积,Nzoia河流域容易退化。本研究的目的是建立Nzoia河流域的土壤侵蚀危害模型并估算其产沙量。流域数据库由90 m DEM、LandSat图像、降雨和土壤数据组成。模拟RUSLE模型因子(R、K、LS、C)使用ArcGIS 10.1中的栅格计算器相乘。得到Nzoia河流域土壤侵蚀危险度图,年平均土壤流失率为0.51,最大土壤流失率为8.84 Mton ha-1 year -1。这意味着年均土壤流失量为6.579 × 105亿吨/年。泥沙输沙比(SDR)为0.121,表明流域被水侵蚀的土壤中有87.9%在到达流域出口之前沉积。估算的年平均产沙量为0.06亿吨-1。土壤侵蚀模拟结果表明,Nzoia河流域在空间上呈现出不同的侵蚀速率。RUSLE因子之间的相互作用对年平均土壤流失率有较大影响。土壤流失率高的地区与年度耕地、森林砍伐和高海拔地区密切相关。土壤流失率低可归因于土壤保持措施和保护区,如狩猎公园。因此,Nzoia河流域土壤流失与土地利用类型之间存在着密切的耦合关系。应采用可持续的土地利用做法来支持保护方案,以减轻土壤侵蚀、防止泥沙淤积和减少河道的泥沙产量。
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