geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3248Research ArticleСтатьиArticleЭрозия на равнинах Восточной ЕвропыErosion on the plains of Eastern EuropeДедковА. П.DedkovA. P.МозжеринВ. И.MoszherinV. I.Казанский государственный университетРоссия1996200320230239Copyright © Дедков А.П., Мозжерин В.И., 20232023Дедков А.П., Мозжерин В.И.Dedkov A.P., Moszherin V.I.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/3248

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.

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.

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The authors declare that there are no conflicts of interest present.