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Freezing and Ice Growth in Frost-Susceptible Soils
Abstract A model for energy transfer, and freezing and thawing of soils is described first. This model is then incorporated into a description of heaving in frost-susceptible soils. Frost heaving is caused by formation of ice lenses, a result of transfer of unfrozen water and freezing at the cold side of the frozen fringe. The description of frost heave presented here is based on a porosity rate function. This description does not model formation of individual ice lenses; rather, it yields the average growth in porosity due to growth of ice. Application of the model is illustrated in examples of a chilled gas pipeline and a retaining wall with frost-susceptible backfill.
Freezing and Ice Growth in Frost-Susceptible Soils
Abstract A model for energy transfer, and freezing and thawing of soils is described first. This model is then incorporated into a description of heaving in frost-susceptible soils. Frost heaving is caused by formation of ice lenses, a result of transfer of unfrozen water and freezing at the cold side of the frozen fringe. The description of frost heave presented here is based on a porosity rate function. This description does not model formation of individual ice lenses; rather, it yields the average growth in porosity due to growth of ice. Application of the model is illustrated in examples of a chilled gas pipeline and a retaining wall with frost-susceptible backfill.
Freezing and Ice Growth in Frost-Susceptible Soils
Michalowski, Radoslaw L. (author) / Zhu, Ming (author)
2007-01-01
13 pages
Article/Chapter (Book)
Electronic Resource
English
Freeze Soil , Cold Side , Unfrozen Water , Volumetric Heat Capacity , Initial Temperature Distribution Physics , Soft and Granular Matter, Complex Fluids and Microfluidics , Continuum Mechanics and Mechanics of Materials , Building Materials , Geoengineering, Foundations, Hydraulics , Numerical and Computational Physics
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