1963
DOI: 10.1139/t63-004
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Volume Changes in Undisturbed Clay Profiles in Western Canada

Abstract: /npsi/ctrl?lang=en http://nparc.cisti-icist.nrc-cnrc.gc.ca/npsi/ctrl?lang=fr Access and use of this website and the material on it are subject to the Terms and Conditions set forth at

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Cited by 14 publications
(2 citation statements)
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“…Swelling and shrinkage in the expansive Regina clay depend on the following distinct but interrelated parameters: (i) soil geology and geotechnical properties [13,14]; (ii) ground cover and vegetation type [15,16]; (iii) seasonal weather and environmental conditions [17,18]; and (iv) hydrologic conditions and depth below surface [19,20]. Based on these factors, a simplified approach was adopted for the selection of parameters affecting volume changes in the expansive clay.…”
Section: Modeling Of Bayesian Belief Network 21 Parameter Selectionmentioning
confidence: 99%
“…Swelling and shrinkage in the expansive Regina clay depend on the following distinct but interrelated parameters: (i) soil geology and geotechnical properties [13,14]; (ii) ground cover and vegetation type [15,16]; (iii) seasonal weather and environmental conditions [17,18]; and (iv) hydrologic conditions and depth below surface [19,20]. Based on these factors, a simplified approach was adopted for the selection of parameters affecting volume changes in the expansive clay.…”
Section: Modeling Of Bayesian Belief Network 21 Parameter Selectionmentioning
confidence: 99%
“…Jones and Holtz, (1973) showed the volume changes in clay, because of variations in moisture content, occur within about 30 ft of the ground surface. However, most changes that cause engineering problems take place at depths of less than 10 ft (Hamilton, 1963;Gromko, 1974). My-W is mostly saturated throughout the year since water logging capability and availability of water; the shrink-swell behaviour is very limited.…”
Section: Swell Potential Of Soilsmentioning
confidence: 99%