ОЦЕНКА ГРАНИЧНЫХ УСЛОВИЙ ФОРМИРОВАНИЯ РУСЕЛ РАЗНЫХ ТИПОВ НА РЕКАХ АЛТАЙСКОГО РЕГИОНА (БАССЕЙН ВЕРХНЕЙ ОБИ)

dc.contributor.author	Смирнова В.Г.
dc.contributor.author	Чалов Р.С.
dc.date.accessioned	2022-05-08T02:20:19Z
dc.date.available	2022-05-08T02:20:19Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=17345328
dc.identifier.citation	Геоморфология, 2004, , 2, 68-73
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/37435
dc.description.abstract	On the base of QI-diagram analysis the formation of different types of channels was considered: for plain rivers, mountain rivers, incised rivers and rivers with broad flood plain. Heterogeneous approximations of boundary lines, dividing point fields on the QI-diagrams, corresponding to different channel types, were revealed. Authors argue that incised channels appear at maximal intensity of flow; branching channels occur on rivers with average maximum discharge more than 50 m 3/sec, which is characteristic for big rivers.
dc.title	ОЦЕНКА ГРАНИЧНЫХ УСЛОВИЙ ФОРМИРОВАНИЯ РУСЕЛ РАЗНЫХ ТИПОВ НА РЕКАХ АЛТАЙСКОГО РЕГИОНА (БАССЕЙН ВЕРХНЕЙ ОБИ)
dc.type	Статья
dc.subject.udc	551.435.11(282.251.1)

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