PDFTech ReportRC-16192010-0294Frost susceptible soilFreeze thaw durabilityMathematical predictionFrost heavingFrostDepthMichiganMichigan. Dept. of Transportation. Office of Research AdministrationBaladi, GilbertRajaei, PegahMichigan State University. Dept. of Civil and Environmental EngineeringUS Transportation CollectionFrost depth is an essential factor in design of various transportation infrastructures. In frostsusceptible soils, as soils freezes, water migrates through the soil voids below the freezing linetowards the freezing front and causes excessive heave. The excessive heave can cause instabilityissues in the structure, therefore predicting the frost depth and resulting frost heave accurately canplay a major role in the design. Th...
Freezing and thawing of soil is a common occurrence throughout the world. Indeed, approximately 50% ...
AbstractThis paper first presents a simple frost heave model. Frost heave is assumed to be caused by...
Phase change of the water in the soil skeleton under cold climate conditions (also known as frost ac...
The purpose of this study is to develop numerical models and tools to simulate the processes of free...
The failure of earth structures subjected to freeze-thaw frequently occurs in seasonal cold regions ...
The freeze–thaw process controls several hydrologic processes, including infiltration, runoff, and s...
The freeze-thaw process controls several hydrologic processes including infiltration, runoff, and so...
Publisher Copyright: © Published under licence by IOP Publishing Ltd. Copyright: Copyright 2021 Else...
More than a third of the Earth's surface is subject to seasonal or prolonged soil frosts, and the re...
Frost-susceptible soils are characterized by their sensitivity to freezing that is manifested in hea...
Frost heave and thaw weakening are two common concerns in designing and constructing roads throughou...
Interest in permafrost, or seasonally frozen ground, has been increasing over the last decades. Near...
Frost heave is a common phenomenon in the Arctic, where soil expands in the direction of heat loss d...
US Transportation Collection2021PDFTech ReportCetin, BoraCetin, KristenEdil, Tuncer B.Mitra, Debrudr...
Graduation date: 1988Freeze/thaw cycles are numerous in agricultural soils of the Pacific Northwest....
Freezing and thawing of soil is a common occurrence throughout the world. Indeed, approximately 50% ...
AbstractThis paper first presents a simple frost heave model. Frost heave is assumed to be caused by...
Phase change of the water in the soil skeleton under cold climate conditions (also known as frost ac...
The purpose of this study is to develop numerical models and tools to simulate the processes of free...
The failure of earth structures subjected to freeze-thaw frequently occurs in seasonal cold regions ...
The freeze–thaw process controls several hydrologic processes, including infiltration, runoff, and s...
The freeze-thaw process controls several hydrologic processes including infiltration, runoff, and so...
Publisher Copyright: © Published under licence by IOP Publishing Ltd. Copyright: Copyright 2021 Else...
More than a third of the Earth's surface is subject to seasonal or prolonged soil frosts, and the re...
Frost-susceptible soils are characterized by their sensitivity to freezing that is manifested in hea...
Frost heave and thaw weakening are two common concerns in designing and constructing roads throughou...
Interest in permafrost, or seasonally frozen ground, has been increasing over the last decades. Near...
Frost heave is a common phenomenon in the Arctic, where soil expands in the direction of heat loss d...
US Transportation Collection2021PDFTech ReportCetin, BoraCetin, KristenEdil, Tuncer B.Mitra, Debrudr...
Graduation date: 1988Freeze/thaw cycles are numerous in agricultural soils of the Pacific Northwest....
Freezing and thawing of soil is a common occurrence throughout the world. Indeed, approximately 50% ...
AbstractThis paper first presents a simple frost heave model. Frost heave is assumed to be caused by...
Phase change of the water in the soil skeleton under cold climate conditions (also known as frost ac...