Laboratory research of snow melting as component of seasonal process of deformations stream channel

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Abstract


A laboratory study of the process of continuous snowmelt and subsequent infiltration of meltwater into the soil, depending on the properties (different initial density, layer thickness and temperature) of snow. We consider the impact of storm flows in the process of thawing.

About the authors

I I Gritsuk

Peoples’ Friendship University of Russia

Email: grizli2881@mail.ru
Department of hydraulic and hydrothechnical building Russian Academy of Sciences Water Problems Institute

V K Debolskiy

Russian Academy of Sciences Water Problems Institute

Email: vdebolsky@mail.ru

O Ya Maslikova

Russian Academy of Sciences Water Problems Institute

Email: oksana68@mail.ru

N K Ponomarev

Peoples’ Friendship University of Russia

Email: rudneng@mail.ru
Department of hydraulic and hydrothechnical building

E K Sinichenko

Peoples’ Friendship University of Russia

Email: eks47@mail.ru
Department of hydraulic and hydrothechnical building

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Copyright (c) 2013 Грицук И.И., Дебольский В.К., Масликова О.Я., Пономарёв Н.К., Синиченко Е.К.

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This work is licensed under a Creative Commons Attribution 4.0 International License.

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