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contributor authorS. McKeown
contributor authorJ. I. Clark
contributor authorD. Matheson
date accessioned2017-05-08T21:13:40Z
date available2017-05-08T21:13:40Z
date copyrightSeptember 1988
date issued1988
identifier other%28asce%290887-381x%281988%292%3A3%28111%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/43480
description abstractThe depth of frost and ground temperatures were monitored on a regular basis between 1983 and 1985 at 12 locations in Tumbler Ridge, British Columbia. The soil is dry gravel which has a moisture content of 1.5 to 4%. The maximum depth of frost recorded was 3.98 m for a winter having 1,430 ° C‐days. Back calculation using the Stefan equation yielded
publisherAmerican Society of Civil Engineers
titleFrost Penetration and Thermal Regime in Dry Gravel
typeJournal Paper
journal volume2
journal issue3
journal titleJournal of Cold Regions Engineering
identifier doi10.1061/(ASCE)0887-381X(1988)2:3(111)
treeJournal of Cold Regions Engineering:;1988:;Volume ( 002 ):;issue: 003
contenttypeFulltext


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