Transport coefficients and pressure conditions for growth of ice lens in frozen soil
In this paper, the transport of sub-cooled water across a partially frozen soil matrix (frozen fringe) caused by a temperature difference over the fringe, is described using non-equilibrium thermodynamics. A set of coupled transport equations of heat and mass is presented; implying that, in the froz...
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Veröffentlicht in: | Acta geotechnica 2021-07, Vol.16 (7), p.2231-2239 |
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Sprache: | eng |
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