Accounting for mudflow genesis in preliminary assessment of the maximum volume of solid mudflow sediments in the North Caucasus
- 作者: Zalikhanov M.C.1, Kondratieva N.V.1, Adzhiev A.K.1, Razumov V.V.1
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隶属关系:
- High-Mountain Geophysical Institute
- 期: 卷 470, 编号 1 (2016)
- 页面: 965-967
- 栏目: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/188911
- DOI: https://doi.org/10.1134/S1028334X16090166
- ID: 188911
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详细
The area of investigation was subject to multifactor analysis of the relationship between the maximum amount of mudflow solid sediments (W) and parameters such as the mudflow basin area (S), average channel slope (α), and mudflow channel length (L). They were used to obtain analytical expressions in order to approximate the W(S, L, α) relation based on the mudflow genesis and source height. Statistical data on mudflow manifestations in different basins in the North Caucasus covering more than fifty years were used to obtain the analytical expressions in order to assess the maximum volume of mudflow solid sediments.
作者简介
M. Zalikhanov
High-Mountain Geophysical Institute
Email: adessa1@yandex.ru
俄罗斯联邦, Roshydromet, Nalshik
N. Kondratieva
High-Mountain Geophysical Institute
Email: adessa1@yandex.ru
俄罗斯联邦, Roshydromet, Nalshik
A. Adzhiev
High-Mountain Geophysical Institute
编辑信件的主要联系方式.
Email: adessa1@yandex.ru
俄罗斯联邦, Roshydromet, Nalshik
V. Razumov
High-Mountain Geophysical Institute
Email: adessa1@yandex.ru
俄罗斯联邦, Roshydromet, Nalshik
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