斯威士兰中部地区土壤侵蚀调查

R.P.C. Morgan, R.J. Rickson, K. McIntyre, T.R. Brewer, H.J. Altshul
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引用次数: 24

摘要

在过去的20年里,斯威士兰中部地区的土壤侵蚀严重恶化。大部分侵蚀发生在深部崩积和腐殖岩物质上,并与山谷两侧的凸坡断裂和回淤肩有关。虽然侵蚀的风险似乎反映了景观的自然不稳定性,但土地的使用方式决定了问题的最终严重性。就侵蚀评估而言,土地系统可以作为功能单元。侵蚀最严重的土地发生在Manzini、Jabuleni、Lobamba和Chibidze土地系统内。通用土壤流失方程(USLE)和南部非洲土壤流失估算器(SLEMSA)对土壤流失率给出了截然不同的估计,但没有可用的信息来验证或反驳这些预测。
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Soil erosion survey of the central part of the Swaziland Middleveld

Soil erosion has worsened considerably in the Middleveld of Swaziland over the last 20 years. Most of the erosion has occurred on deep colluvial and saprolitic materials and is associated with convex-slope breaks and rejuvenation shoulders on valley sides. Although the risk of erosion seems to reflect natural instability in the landscape, the way in which the land is used determines the ultimate severity of the problem. Land systems can serve as functional units as far as erosion assessment is concerned. The most severely eroded land occurs within the Manzini, Jabuleni, Lobamba and Chibidze land systems. The universal soil loss equation (USLE) and the soil loss estimator for southern Africa (SLEMSA) give vastly different estimates of the rate of soil loss but no information is available to validate or refute the predictions.

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Publisher's note Soil erosion in Swaziland: A synthesis Soil erosion and sedimentation in Swaziland: an introduction Factors affecting changes in erosion status in the Swaziland Middleveld A rainfall simulation study of soil erosion on rangeland in Swaziland
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