geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3485Research ArticleМетодика научных исследованийScientific Research MethodsМодель для расчета морфометрии стабильного оврагаModel for calculation of stabilized gully morphologyСидорчукА. Ю.SidorchoukA. Yu.Московский государственный университет имени М.В.Ломоносова, географический факультетRussian Federation199818122023024352Copyright © Сидорчук А.Ю., 20232023Сидорчук А.Ю.Sidorchouk A.Y.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/3485

For taking erosion-control measures the maximum final size of gully is important. Static model for calculating the longitudinal and transversal profiles is proposed. Gully is supposed to be stabile, formed in cohesive ground, the stream velocity - to be higher than critical one, at which accumulation of little particles begins, and at the same time to be lower than the scouring rate. In the model the whole range of water discharge is taken into account. The corresponding computer program has been compiled.

For taking erosion-control measures the maximum final size of gully is important. Static model for calculating the longitudinal and transversal profiles is proposed. Gully is supposed to be stabile, formed in cohesive ground, the stream velocity - to be higher than critical one, at which accumulation of little particles begins, and at the same time to be lower than the scouring rate. In the model the whole range of water discharge is taken into account. The corresponding computer program has been compiled.

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