Эрозия на равнинах Восточной Европы
Аннотация
Three zones have been distinguished on the plains of Eastern Europe based on suspended load and gully erosion: the north-western zone of weak erosion (rate of suspended load discharge averages to 5.6 t/km2 year, gully density up to 200 m/km2, channel erosion and sheet wash prevail), middle zone of intense erosion (44 t/km2 year, gully density in excess of 200 m/km2, sheet wash and gully erosion prevail), south-eastrn zone of weak erosion (8.1 t/km2 year, less than 200 m/km2). Natural and anthropogenic factors are considered which account for the identified distinctions.
Об авторах
А. П. ДедковРоссия
В. И. Мозжерин
Россия
Рецензия
Для цитирования:
Дедков А.П., Мозжерин В.И. Эрозия на равнинах Восточной Европы. Геоморфология и палеогеография. 1996;(2):3-9.
For citation:
Dedkov A.P., Moszherin V.I. Erosion on the plains of Eastern Europe. Geomorfologiya i Paleogeografiya. 1996;(2):3-9.