斯威士兰草原土壤侵蚀的降雨模拟研究

R.P.C. Morgan, K. McIntyre, A.W. Vickers, J.N. Quinton, R.J. Rickson
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引用次数: 45

摘要

对斯威士兰Ntondozi地区草地的降雨模拟研究表明,土壤流失量随着植被覆盖的增加呈指数下降。植被通过增加土壤入渗能力发挥重要的水文控制作用,进而影响径流的发生时间和持续时间。植被对土壤保护和土壤强度的预期效果未得到证实。相反,在单个风暴中发生的土壤流失量似乎取决于地表松散物质的供应,这些物质可以通过径流运输。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A rainfall simulation study of soil erosion on rangeland in Swaziland

Rainfall simulation studies on rangeland in the Ntondozi area of Swaziland showed that soil loss decreased exponentially with increasing vegetation cover. Vegetation exerted an important hydrological control by increasing the infiltration capacity of the soil which, in turn, influenced the time to and duration of runoff. The expected effects of vegetation on soil protection and soil strength were not demonstrated. Instead, the amount of soil loss occurring in an individual storm appeared to depend on the supply of loose material on the surface which could be transported by the runoff.

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