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JOURNALS // News of the Kabardino-Balkarian Scientific Center of the Russian Academy of Sciences // Archive

News of the Kabardin-Balkar scientific center of RAS, 2012 Issue 1, Pages 43–47 (Mi izkab529)

This article is cited in 4 papers

SCIENCES ABOUT THE EARTH

About the possible mechanism of formation of sill (mudstream) flows

E. V. Kyula, D. R. Dzhappuevb

a Kabardin-Balkar Scientific Center of the Russian Academy of Sciences, Center of geographical researches, 360002, ÊÁÐ, Nalchik, 2, Balkarova street
b Elbrus foothills National park, 361603, ÊBR, settlement Elbrus, 4, Lesnaya street

Abstract: In the article the mechanism of formation of sill flows is considered. The sill formation factors of erosion - sill process are allocated. Authors formulated a hypothesis about conditions of development of a water-transport stream into sill torrent. Types of streams depending on a angle of bedding of possible sill materials (PSM) and the water expense are allocated. Dependences are defined: 1) a limiting weight saturation by a stream of a firm material from a channel bias; 2) between the value of density of sill mass and a bias of sell channels

Keywords: sill flow, sill forming factors, erosion-shift sill process, critical expense of a water stream, critical bias of sill channels, high saturation of an earth flow, density of sill weights.

UDC: 551.311.21

Received: 13.10.2011



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