Ice lensing in layered soils
Copyright policy )Ice lensing in layered soils
The ice lensing phenomenon in layered soils, a condition that simulates the process of ice growth in varved soils, has been studied experimentally. Under the limited conditions of layer thicknesses, soils used, freezing rates, and moisture conditions, ice lenses formed at the face of the fine-textured (clay) layer when it was encountered by the freezing plane. Only minor heaving occurred in the coarse-textured (silt) layer when its thickness was increased. Key words: frost action, ice lensing, frost heaving, varved soils, layered soils.
silt, gel, sol argileux, sol, frost heaving, ice, ice lensing, varved soils, layered soils, foisonnement par le gel, frozen soils, clay soils, sédimentation, limon, glace, frost, sedimentation, frost action, pergélisol, soils, sol gelé, permafrost
silt, gel, sol argileux, sol, frost heaving, ice, ice lensing, varved soils, layered soils, foisonnement par le gel, frozen soils, clay soils, sédimentation, limon, glace, frost, sedimentation, frost action, pergélisol, soils, sol gelé, permafrost
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