Accounting for mudflow genesis in preliminary assessment of the maximum volume of solid mudflow sediments in the North Caucasus


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

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

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2016