The purpose of this study is to develop numerical models and tools to simulate the processes of freezing and thawing in soils and to predict frost heave associated with freezing of frost-susceptible soils. A numerical procedure for heat transfer in freezing and thawing soils is presented first. The frozen soil is a mixture of solid particles, unfrozen water, ice, and air. The multi-phase nature and the unique role of pore water complicate the heat transfer process in freezing or thawing soils. A major characteristic of the pore water is its presence in frozen soil even at temperatures well below freezing. As a result, the latent heat of fusion of water is released or absorbed over a range of temperatures below freezing, rather than at on...
Progressive freezing of unsaturated soil induces moisture migration from warm to cold regions. The ...
Progressive freezing of unsaturated soil induces moisture migration from warm to cold regions. The ...
This paper introduces a thermo-hydro-mechanical computational model for freezing and thawing in poro...
Frost-susceptible soils are characterized by their sensitivity to freezing that is manifested in hea...
A laboratory study of infiltration rates into frozen and unfrozen fine sand, including temperature e...
A laboratory study of infiltration rates into frozen and unfrozen fine sand, including temperature e...
Frost heaving is a major cause of damage to infrastructures structures in cold regions. While signif...
A numerical method is presented that models the coupled flow of heat, water, and solutes as unsatura...
The freeze-thaw process controls several hydrologic processes including infiltration, runoff, and so...
This paper investigates the thermo-hydro-mechanical (THM) behaviour of soils subjected to seasonal t...
A generalized model for secondary frost heave in freezing fine-grained soils is presented and discus...
Frost heave is a common phenomenon in the Arctic, where soil expands in the direction of heat loss d...
The freeze–thaw process controls several hydrologic processes, including infiltration, runoff, and s...
Although much effort has been made to develop various frost heave models in the past decades, a simp...
Permafrost has been thawing faster due to climate change which would release greenhouse gases, chang...
Progressive freezing of unsaturated soil induces moisture migration from warm to cold regions. The ...
Progressive freezing of unsaturated soil induces moisture migration from warm to cold regions. The ...
This paper introduces a thermo-hydro-mechanical computational model for freezing and thawing in poro...
Frost-susceptible soils are characterized by their sensitivity to freezing that is manifested in hea...
A laboratory study of infiltration rates into frozen and unfrozen fine sand, including temperature e...
A laboratory study of infiltration rates into frozen and unfrozen fine sand, including temperature e...
Frost heaving is a major cause of damage to infrastructures structures in cold regions. While signif...
A numerical method is presented that models the coupled flow of heat, water, and solutes as unsatura...
The freeze-thaw process controls several hydrologic processes including infiltration, runoff, and so...
This paper investigates the thermo-hydro-mechanical (THM) behaviour of soils subjected to seasonal t...
A generalized model for secondary frost heave in freezing fine-grained soils is presented and discus...
Frost heave is a common phenomenon in the Arctic, where soil expands in the direction of heat loss d...
The freeze–thaw process controls several hydrologic processes, including infiltration, runoff, and s...
Although much effort has been made to develop various frost heave models in the past decades, a simp...
Permafrost has been thawing faster due to climate change which would release greenhouse gases, chang...
Progressive freezing of unsaturated soil induces moisture migration from warm to cold regions. The ...
Progressive freezing of unsaturated soil induces moisture migration from warm to cold regions. The ...
This paper introduces a thermo-hydro-mechanical computational model for freezing and thawing in poro...