The Features of Snowmelt Runoff Waters in Presalairya in an Extremely Snow-rich Hydrological Year
A. TANASIENKO, A. CHUMBAEV
Pages: 907–919
Abstract
It is shown that the depth and degree of frost penetration in the leached chernozem (black soil) of Presalairya were minimal in an extremely snow-rich hydrological year when the amount of water accumulated in snow was twice as large as the norm.
