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Геоморфология и палеогеография

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Движение масс по склонам и почвы

Аннотация

The paper discusses mass movement influence on morphological and chemical properties of soils. The mass movements: 1) provide homogeneity of parent material under conditions of complicate geological structure, 2) f acilitate the mineral mass weathering which accounts for difference in the chemical composition between slope formations and solid rocks; 3) control the vertical differentiation of soil profile (defluction permits the morphological differentiation of soil, slow solifluction determines a homogenous brown soil profile which is given an informal name «creepozem»), 4) mass movements on slopes influence the long-existing (conservative) properties (morphology, general chemical composition) while more dynamic characteristics (humus, pH, absorbed bases) have time to differentiate even under relatively «high» rate of the mass movement.

Об авторах

В. В. Беркгаут
Почвенный институт ВАСХНИЛ
Россия


Н. И. Белоусова
Почвенный институт ВАСХНИЛ
Россия


Рецензия

Для цитирования:


Беркгаут В.В., Белоусова Н.И. Движение масс по склонам и почвы. Геоморфология. 1985;(1):57-65.

For citation:


Berkgaut V.V., Belousova N.I. Mass movement on slopes and soils. Geomorfologiya. 1985;(1):57-65.

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ISSN 2949-1789 (Print)
ISSN 2949-1797 (Online)