geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-1655Research ArticleНаучные сообщенияShort communicationsНекоторые характеристики оврагообразовательного процесса в предгорьях КавказаSome characteristics of gullies formation in the Сaucasian foothillsВиноградоваН. Н.VinogradovaN. N.СамойловаА. А.SamoilovaA. A.Московский государственный университет имени М.В.Ломоносова, Географический факультетРоссия19901605202201Геоморфология4549Copyright © Виноградова Н.Н., Самойлова А.А., 20222022Виноградова Н.Н., Самойлова А.А.Vinogradova N.N., Samoilova A.A.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/1655

Changes in a gully's longitudinal profile have been recorded by stationary observations. The analysis of the data permitted to conclude that the gully's development had achieved the erosional equilibrium stage. It has been confirmed by the calculated equilibrium profile which appeared to be close to the natural one. The time of the gully's development and the quantity of solid matter brought by the gully into drainage network have been estimated.

Changes in a gully's longitudinal profile have been recorded by stationary observations. The analysis of the data permitted to conclude that the gully's development had achieved the erosional equilibrium stage. It has been confirmed by the calculated equilibrium profile which appeared to be close to the natural one. The time of the gully's development and the quantity of solid matter brought by the gully into drainage network have been estimated.

References

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