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Record #126407:

The relationship between ice intrusion temperature and confined pressure / Ruijie Chen, Kaoru Horiguchi.

Title: The relationship between ice intrusion temperature and confined pressure / Ruijie Chen, Kaoru Horiguchi.
Author(s): Chen, Ruijie.
Horiguchi, Kaoru.
Date: 1993.
Publisher: Wushan, Guangzhou: South China University of Technology Press
In: Permafrost. Sixth International Conference. Proceedings (Vol. 2), July 5-9, 1993, Beijing China. (1993.),
Abstract: Ice intrusion temperature is temperature near or below 0°C at which freezing of pore water can advance continuously without water migration, and unfrozen water content and hydraulic conductivity of soil decrease sharply. Experiments indicated that ice intrusion temperature decreases with increase of confined pressure, i.e. there are different ice intrusion temperatures for different pore sizes because of different degrees of compression.
Notes:

In: Permafrost. Sixth International Conference. Proceedings (Vol. 2), July 5-9, 1993, Beijing China / International Conference on Permafrost.

Keywords: 551.34 -- Geocryology. Frozen ground.
551.343.7 -- Frost, soil moisture and surface water, effect on movement of.
551.345.2 -- Permafrost, formation and decay.
E8 -- Glaciology: frost action and permafrost.
SPRI record no.: 126407

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245 14 ‡aThe relationship between ice intrusion temperature and confined pressure /‡cRuijie Chen, Kaoru Horiguchi.
260 ## ‡aWushan, Guangzhou :‡bSouth China University of Technology Press,‡c1993.
300 ## ‡ap. 1067-1069 :‡bdiags.
500 ## ‡aIn: Permafrost. Sixth International Conference. Proceedings (Vol. 2), July 5-9, 1993, Beijing China / International Conference on Permafrost.
520 3# ‡aIce intrusion temperature is temperature near or below 0°C at which freezing of pore water can advance continuously without water migration, and unfrozen water content and hydraulic conductivity of soil decrease sharply. Experiments indicated that ice intrusion temperature decreases with increase of confined pressure, i.e. there are different ice intrusion temperatures for different pore sizes because of different degrees of compression.
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.343.7 -- Frost, soil moisture and surface water, effect on movement of.‡2udc
650 07 ‡a551.345.2 -- Permafrost, formation and decay.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
700 1# ‡aHoriguchi, Kaoru.
773 0# ‡7m2am ‡aInternational Conference on Permafrost. ‡tPermafrost. Sixth International Conference. Proceedings (Vol. 2), July 5-9, 1993, Beijing China. ‡dWushan, Guangzhou : South China University of Technology Press, 1993. ‡wSPRI-204174
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