Variations in the Porosity of Frozen Ground Produced by Thawing (K Metodike Opredeleniya Koeffitsientov Ottaivaniya i Uplotneniya Merzlykh Gruntov)

The experiments conducted with quartz sand, blanket loam and varved clay fully confirm the theory previously expressed by N.A. Tsytovich concerning the rectilinear dependence between the variation in porosity factor and the value for pressure on soil during thawing. (Author) Draft trans. of Akademiy...

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Bibliographic Details
Main Author: Shusherina ,E. P.
Other Authors: COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Format: Text
Language:English
Published: 1972
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0739962
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0739962
Description
Summary:The experiments conducted with quartz sand, blanket loam and varved clay fully confirm the theory previously expressed by N.A. Tsytovich concerning the rectilinear dependence between the variation in porosity factor and the value for pressure on soil during thawing. (Author) Draft trans. of Akademiya Nauk SSSR. Institut Merzlotovedeniya. Materialy po Laboratornym Issledovaniyam Merzlykh Gruntov, n1 p118-134 1953.