Regularities of the distribution of eroded and aggraded soddy-podzolic soils on slopesстатья
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Статья опубликована в журнале из перечня ВАК
Дата последнего поиска статьи во внешних источниках: 6 октября 2021 г.
Аннотация: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.