СТРУКТУРА РУСЛОВОГО РЕЛЬЕФА НИЖНЕЙ ВОЛГИ
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dc.contributor.author | Сидорчук А.Ю. | |
dc.date.accessioned | 2022-12-03T09:10:06Z | |
dc.date.available | 2022-12-03T09:10:06Z | |
dc.date.issued | 2005 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=9142774 | |
dc.identifier.citation | Геоморфология, 2005, , 2, 86-96 | |
dc.identifier.issn | 0435-4281 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/40705 | |
dc.description.abstract | The hierarchical classification of Lower Volga channel landforms is put forward. The classification consists of 8 complexes and 5 classes. The class of nanoforms includes riffles; microforms - dunes and zastrugas; mezoforms -sand waves and alternate bars; macroforms - big meanders and large ramification junctions; megaforms - ramifica-tions with parallel arms or the river. The main channel of Volga and its branch - Akhtuba form a parallel-channel system. Empirical probability density of channel forms length (for each class) may be fitted well by Gamma distribu-tion; the height may by fitted by Weibull distribution. | |
dc.title | СТРУКТУРА РУСЛОВОГО РЕЛЬЕФА НИЖНЕЙ ВОЛГИ | |
dc.type | Статья | |
dc.subject.udc | 551.435.11(282.247.41) |
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