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首页> 外文期刊>Moscow University Soil Science Bulletin >Regularities of the distribution of eroded and aggraded soddy-podzolic soils on slopes.
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Regularities of the distribution of eroded and aggraded soddy-podzolic soils on slopes.

机译：坡面侵蚀和侵蚀的泥质坡积土的分布规律。

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摘要

The distribution of differently eroded soddy-podzolic soils on slopes of different gradients, lengths, and aspects has been studied with the use of a quantitative parameter of slope erodibility K. The latter is calculated as a product of slope gradient in the power of 1.3 and the length of the flow line (m) in the power of 0.5. It is shown that moderately eroded soddy-podzolic soils appear on the slopes of northern and northeastern aspects with K equal to 0.4; on the slopes of southern aspect, this parameter is somewhat lower (0.24). Moderately eroded soils prevail on the slopes of northern and northeastern aspects with K equal to 0.7.
机译：利用斜坡可蚀性定量参数 K 研究了坡度，坡度和坡度不同的坡面不同侵蚀性坡地土壤的分布。后者的计算公式是斜率梯度为1.3的幂与流线长度（m）的幂为0.5的乘积。结果表明，北部和东北部斜坡上出现了中等侵蚀的泥质坡积土， K 等于0.4。在南部坡度上，此参数较低（0.24）。在北部和东北部的坡度上普遍存在中度侵蚀土壤， K 等于0.7。

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