It is possible to construct numerical models of the ice segregation process. However, the model is a discrete approximation of a nonlinear continuous process and thus is subject to somewhat more pronounced effects of node geometry and calculation frequency than linear models. The model more closely simulates natural frozen soil structure when vapor phase transport is included in the model structure. An iteration frequency of 10 s appeared sufficient to yield realistic results with the exponentially spaced node geometry employed in these tests.Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/23588/1/0000550.pd
The presence of ice in soil dramatically alters soil hydrologic and thermal properties. Despite this...
Frost-susceptible soils are characterized by their sensitivity to freezing that is manifested in hea...
A characteristic of frozen ground is a tendency to form banded sequences of particle-free ice lenses...
Step functions of normal frost front advance in dry and wet soils are reviewed and used to introduce...
In recent studies, vapour transfer is reported to lead to remarkable frost heave in unsaturated soil...
A numerical method is presented that models the coupled flow of heat, water, and solutes as unsatura...
This paper investigates the thermo-hydro-mechanical (THM) behaviour of soils subjected to seasonal t...
The freeze-thaw process controls several hydrologic processes including infiltration, runoff, and so...
The ground ice content in cold environments influences the permafrost thermal regime and the thaw tr...
Soil surface temperature, net radiation and surface heave are used to evaluate a computer simulation...
The freeze–thaw process controls several hydrologic processes, including infiltration, runoff, and s...
The purpose of this study is to develop numerical models and tools to simulate the processes of free...
Frost heave can have a very destructive impact on infrastructure in permafrost regions. The complexi...
A laboratory study of infiltration rates into frozen and unfrozen fine sand, including temperature e...
Interest in permafrost, or seasonally frozen ground, has been increasing over the last decades. Near...
The presence of ice in soil dramatically alters soil hydrologic and thermal properties. Despite this...
Frost-susceptible soils are characterized by their sensitivity to freezing that is manifested in hea...
A characteristic of frozen ground is a tendency to form banded sequences of particle-free ice lenses...
Step functions of normal frost front advance in dry and wet soils are reviewed and used to introduce...
In recent studies, vapour transfer is reported to lead to remarkable frost heave in unsaturated soil...
A numerical method is presented that models the coupled flow of heat, water, and solutes as unsatura...
This paper investigates the thermo-hydro-mechanical (THM) behaviour of soils subjected to seasonal t...
The freeze-thaw process controls several hydrologic processes including infiltration, runoff, and so...
The ground ice content in cold environments influences the permafrost thermal regime and the thaw tr...
Soil surface temperature, net radiation and surface heave are used to evaluate a computer simulation...
The freeze–thaw process controls several hydrologic processes, including infiltration, runoff, and s...
The purpose of this study is to develop numerical models and tools to simulate the processes of free...
Frost heave can have a very destructive impact on infrastructure in permafrost regions. The complexi...
A laboratory study of infiltration rates into frozen and unfrozen fine sand, including temperature e...
Interest in permafrost, or seasonally frozen ground, has been increasing over the last decades. Near...
The presence of ice in soil dramatically alters soil hydrologic and thermal properties. Despite this...
Frost-susceptible soils are characterized by their sensitivity to freezing that is manifested in hea...
A characteristic of frozen ground is a tendency to form banded sequences of particle-free ice lenses...