АНАЛИЗ ИНТЕНСИВНОСТИ ДЕФОРМАЦИЙ РУСЛА В РАЗНЫЕ ФАЗЫ ВОДНОГО РЕЖИМА (НА ПРИМЕРЕ УЧАСТКА СРЕДНЕЙ ОБИ)

dc.contributor.author	Каргаполова И.Н.
dc.contributor.author	Сурков В.В.
dc.date.accessioned	2021-12-08T07:10:29Z
dc.date.available	2021-12-08T07:10:29Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=17355776
dc.identifier.citation	Геоморфология, 2003, , 3, 54-61
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/33072
dc.description.abstract	Channel deformation rate at different phases of water regime was analysed. Conditions of sediment accumulation and breaking-up were determined and mobility of sediment was evaluated. The phase of maximum channel deformation intensity corresponds to the moments of channel-forming discharge.
dc.title	АНАЛИЗ ИНТЕНСИВНОСТИ ДЕФОРМАЦИЙ РУСЛА В РАЗНЫЕ ФАЗЫ ВОДНОГО РЕЖИМА (НА ПРИМЕРЕ УЧАСТКА СРЕДНЕЙ ОБИ)
dc.type	Статья
dc.subject.udc	551.435.13(282.251.1)

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