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dc.contributor.author Das, Braja M.
dc.date.accessioned 2019-04-30T09:08:01Z
dc.date.available 2019-04-30T09:08:01Z
dc.date.issued 1988
dc.identifier.citation First published 1983 by Hemisphere Publishing Corporation and McGraw-Hill Second edition published 1997 by Taylor & Francis This edition published 2008 by Taylor & Francis 270 Madison Ave, New York, NY 10016, USA en_US
dc.identifier.isbn 0-203-93584-5
dc.identifier.issn 0–415–42026–1
dc.identifier.uri http://hdl.handle.net/123456789/1229
dc.description The presence of exchangeable cations on the surface of clay particles was discussed in the preceding section en_US
dc.description.abstract A naturally occurring soil sample may have particles of various sizes. Over the years, various agencies have tried to develop the size limits of gravel, sand, silt, and clay. en_US
dc.language.iso en en_US
dc.publisher Taylor & Francis en_US
dc.subject SOIL AGGREGATE, PLASTICITY, AND CLASSIFICATION en_US
dc.subject STRESSES AND STRAINS—ELASTIC EQUILIBRIUM en_US
dc.subject STRESSES AND DISPLACEMENTS IN A SOIL MASS en_US
dc.title Advanced Soil Mechanics en_US
dc.title.alternative Third edition en_US
dc.type Book en_US


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