利用RUSLE和地理空间工具在印度西高止山脉南部热带山地流域进行土壤侵蚀和产沙模拟

A.L. Achu , Jobin Thomas
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引用次数: 1

摘要

基于土壤侵蚀风险制定综合土壤保持战略是流域可持续管理的关键组成部分之一,尤其是在热带山区。本研究计算了热带山区河流流域长期平均年土壤流失量(A)和产沙量(SY)的空间分布,并对土壤侵蚀风险进行了优先排序。在GIS环境中,将修订的通用土壤流失方程(RUSLE)和输沙分布模型(SEDD)模型相结合,以预测西高止山脉南部(印度喀拉拉邦)Karimpuzha河流域(KRB)A和SY的流域内变化。结果表明,平均每年每公顷有9.3 t土壤受到侵蚀,而SY为6.3 t ha−1 y−1(即约占总土壤侵蚀的三分之二)。流域大部分地区(74.2%)的SY较低(即≤5.0 t ha−1 y−1),而土壤侵蚀和迁移过程是一些地区(约6.3 km2)的主要问题。研究结果表明,土地利用/土地覆盖、降雨和地形在控制流域土壤侵蚀风险方面具有重要意义。该研究证明了基于流域水文响应单元(HRU)划定关键侵蚀区的优势,以实施适当的土壤侵蚀管理方案来保护土壤资源。
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Soil erosion and sediment yield modeling in a tropical mountain watershed of the southern Western Ghats, India using RUSLE and Geospatial tools

The development of comprehensive soil conservation strategies, based on the soil erosion risk, is one of the critical components of sustainable river basin management, especially in tropical mountainous regions. The present study computes the spatially distributed longtime average annual soil loss (A) and sediment yield (SY) and prioritizes the soil erosion risk in a tropical mountain river basin. The Revised Universal Soil Loss Equation (RUSLE) and the sediment delivery distributed model (SEDD) models were coupled in the GIS environment to predict the intra-basin variability of the A and SY of the Karimpuzha River Basin (KRB) of the southern Western Ghats (in Kerala, India). The results indicate that, on an average basis, 9.3 t of soil has been eroded per hectare per year, whereas the SY is 6.3 t ha−1 y−1 (i.e., approximately two-thirds of the gross soil erosion). The SY of the majority (74.2%) of the basin area is low (i.e., ≤5.0 t ha−1 y−1), whereas the soil erosion and transport processes are a major concern in some areas (ca. 6.3 km2). The results imply the significance of land use/land cover, rainfall, and topography in controlling the soil erosion risk of the basin. The study demonstrates the advantages of the delineation of the critical erosion areas, based on the hydrologic response units (HRUs) of the basin, to implement appropriate soil erosion management options for conservation of the soil resources.

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