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I.L. Khabibullin (2000)
Ecological Foundation of Land Use while Development and Gas and Condensate Field in Far North
A.S. Lozovskii (1977)
Thermal and Mechanical Interaction of Engineering Structures with Frozen Soils
(2015)
Impact of dynamics of air temperature and snow cover thickness on the ground freezing
(2001)
Fundamentals of Geocryology, Pt. 4, Dynamic Geocryology
A.F. Chudnovskii (1976)
Thermophysics of Soils
M.V. Soldatkin I.L. Khabibullin (2012)
Dynamics of freezing of permafrost seasonally thawed layerVestnik BashGU, 17
S.A. Lobastova I.L. Khabibullin (2007)
Modeling of a thermokarst lake and the assessment of its ecogeocryological dangerVestnik BashGU, 12
(1978)
Some Methods for Numerical Implementation of Multi-Dimensional Boundary-Value Problems in Mathematical Physics
I. Khabibullin, G. Zakirova (2014)
SIMULATION OF THAW FROZEN GROUND UNDER THE INSULATION LAYERS, 19
(2007)
Modeling of a thermokarst lake and the assessment of its ecogeocryological danger, Vestnik BashGU
(2012)
Soldatkin, Dynamics of freezing of permafrost seasonally thawed layer
(2000)
Khabibullin, Ecological Foundation of Land Use while Development and Gas and Condensate Field in Far
(1980)
Heat and Mass Transfer in Rocks at Phase Transitions
(1984)
Thermokarst and Permafrost
(1977)
Lozovskii, Thermal and Mechanical Interaction of Engineering Structures with Frozen Soils
(1979)
Thermophysics of Landscapes
(2002)
Heat exchange between active soil and atmosphere: the oretical and applied aspects
(1980)
Prediction of the Thermal Regime of Frozen Rocks under Natural and Artificial Covers
(2005)
Analytical research of models of termoerosion frozen grounds
Abstract A mathematical model for calculating the distribution of temperature and the dynamics of the phase transfor-mations of water in multilayer systems on permafrost-zone surface is proposed. The model allows one to perform calculations in the annual cycle, taking into account the distribution of temperature on the surface in warm and cold seasons. A system involving four layers, a snow or land cover, a top layer of soil, a layer of thermal-insulation materi-al, and a mineral soil, is analyzed. The calculations by the model allow one to choose the optimal thickness and com-position of the layers which would ensure the stability of structures built on the permafrost-zone surface.
Thermophysics and Aeromechanics – Springer Journals
Published: Jan 1, 2018
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