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 |