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Soil erosion risk assessment of the Keiskamma catchment, South Africa using GIS and remote sensing

机译:使用GIS和遥感技术对南非Keiskamma流域的土壤侵蚀风险进行评估

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摘要

This paper examines the soil loss spatial pat terns in the Keiskamma catchment using the GIS-based Sediment Assessment Tool for Effective Erosion Control (SATEEC) to assess the soil erosion risk of the catchment. SATEEC estimates soil loss and sediment yield within river catchments using the Revised Universal Soil Loss Equation (RUSLE) and a spatially distributed sediment delivery ratio. Vegetation cover in protected areas has a significant effect in curtailing soil loss. The effect of rainfall was noted as two pronged, higher rainfall amounts received in the escarpment promote vegetation growth and vigour in the Amatole mountain range which in turn pos itively provides a protective cover to shield the soil from soil loss. The negative aspect of high rainfall is that it increases the rainfall erosivity. The Keiskamma catchment is predisposed to excessive rates of soil loss due to high soil erodibility, steep slopes, poor conservation practices and low vegetation cover. This soil erosion risk assessment shows that 35% of the catchment is prone to high to extremely high soil losses higher than 25 ton ha~(-1) year~(-1) whilst 65% still experience very low to moderate levels of soil loss of less than 25 ton ha~(-1) year~(-1). Object based classification highlighted the occurrence of enriched valley infill which flourishes in sediment laden ephemeral stream channels. This occurrence increases gully erosion due to overgrazing within ephemeral stream channels. Measures to curb further degradation in the catchment should thrive to strengthen the role of local institutions in controlling conservation practice.
机译:本文使用基于GIS的有效侵蚀控制沉积评估工具(SATEEC)来评估Keiskamma流域的土壤流失空间格局,以评估流域的土壤侵蚀风险。 SATEEC使用经修订的通用土壤流失方程(RUSLE)和空间分布的沉积物输送比估算河流流域内的土壤流失和沉积物产量。保护区的植被覆盖在减少土壤流失方面具有重要作用。降雨的影响被注意到是因为在陡峭的山坡上接收到的两个分支的较高的降雨量促进了Amatole山脉的植被生长和活力,从而反过来提供了保护土壤的保护层,以防止土壤流失。高降雨的不利方面是,它增加了降雨的侵蚀力。 Keiskamma集水区由于高土壤易蚀性,陡峭的坡度,不良的保护措施和低植被覆盖率而导致土壤流失率过高。该土壤侵蚀风险评估表明,超过25吨公顷〜(-1)年〜(-1),有35%的流域容易发生高到极高的土壤流失,而65%的流域仍然有非常低至中等的水土流失水平小于25吨ha〜(-1)年〜(-1)。基于对象的分类突出了富集的山谷填充物的发生,该填充物在充满沉积物的短暂河流中蓬勃发展。由于临时河道内的过度放牧,这种情况加剧了沟壑侵蚀。遏制流域进一步退化的措施应蓬勃发展,以增强地方机构在控制保护实践中的作用。

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  • 来源
    《Environmental earth sciences》 |2012年第7期|p.2087-2102|共16页
  • 作者单位

    Department of Geosciences, Nelson Mandela Metropolitan University, Port Elizabeth, PO Box 77000, South Africa;

    Department of Geosciences, Nelson Mandela Metropolitan University, Port Elizabeth, PO Box 77000, South Africa;

    Department of Regional Infrastructure Engineering,Kangwon National University, Kangwon, Chuncheon, Korea;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    soil erosion; RUSLE; SATEEC GIS remote sensing;

    机译:水土流失;RUSLE;SATEEC GIS遥感;

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