Условия овраг образования в просадочных лессовидных породах
Аннотация
Gully formation in loess-like deposits is usually accompanied by subsidence if porosity coefficient is more than 0.68 and by subsidence and suffusion if the coefficiaent exceeds 1. Granulometry, physical properties and response of the deposits to load determine variety of the gullies types as well as efficiency of the erosion control measures.
Рецензия
Для цитирования:
Ивонин В.М. Условия овраг образования в просадочных лессовидных породах. Геоморфология. 1984;(3):59-65.
For citation:
Ivonin V.M. Conditions of gully formation in loess-like deposits liable to subsidence. Geomorfologiya. 1984;(3):59-65.
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