1967
DOI: 10.1061/jsfeaq.0000982
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Temperature Effects on Clay Soil Consolidation

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Cited by 98 publications
(26 citation statements)
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“…The model was afterwards modified by Picard (1994) who adopted a simpler exponential expression for the variations of isotropic yield stress with temperature. Based on a deeper examination of the experimental results from various authors (Paaswell 1967, Campanella and Mitchell 1968, Plum and Esrig 1969, Demars and Charles 1982, Houston and Lin 1987, Baldi et al 1988, 1991, Eriksson 1989, Tidfors and Sällfors 1989, Towhata et al 1993, proposed a multi-mechanism model able to account better for the effect of OCR on the volume change behaviour of clays under heating. Time-dependent phenomena are significant in deep clays in many underground geotechnical problems (Giraud & Rousset, 1996;Bastiaens et al, 2007) in relation to both the effects of pore water dissipation and of the soil skeleton viscosity.…”
Section: Introductionmentioning
confidence: 99%
“…The model was afterwards modified by Picard (1994) who adopted a simpler exponential expression for the variations of isotropic yield stress with temperature. Based on a deeper examination of the experimental results from various authors (Paaswell 1967, Campanella and Mitchell 1968, Plum and Esrig 1969, Demars and Charles 1982, Houston and Lin 1987, Baldi et al 1988, 1991, Eriksson 1989, Tidfors and Sällfors 1989, Towhata et al 1993, proposed a multi-mechanism model able to account better for the effect of OCR on the volume change behaviour of clays under heating. Time-dependent phenomena are significant in deep clays in many underground geotechnical problems (Giraud & Rousset, 1996;Bastiaens et al, 2007) in relation to both the effects of pore water dissipation and of the soil skeleton viscosity.…”
Section: Introductionmentioning
confidence: 99%
“…Other studies showed that the mechanical behavior of sand-clay mixtures highly depends on mineralogical composition, mineral structure of clay, clay proportions, temperature, and hydrogeological characteristics [42][43][44][45][46][47][48][49][50][51][52][53][54]. Further studies have also investigated the effect of water content [34,55,56], the swelling properties and the suction distribution [34,55,57], the porosity and permeability [56,58], and the volume changes [36] on sand-clay mixtures, pointing out that each of them has non-negligible effects on the behavior of such mixtures.…”
Section: Definition Of Sand-clay Mixturementioning
confidence: 99%
“…As soil is heated under drained conditions, elastic and plastic volume changes may occur due to the expansion and contraction of the soil particles and pore water. Campanella and Mitchell 5 9 (1968) and Paaswell (1967) found that the primary mechanism for plastic volumetric strains during heating of saturated soils is the differential expansion of the water and soil particles.…”
Section: Temperature Effects On the Volume Change And Shear Strength Of Soilsmentioning
confidence: 99%
“…The stress state also plays an important role in the thermal volume change of soils. For example, in saturated soils with overconsolidation ratios (OCRs) greater than 3, elastic expansion is observed during heating and excess pore water pressures are not as significant as in normally consolidated conditions, leading to a negligible change in undrained shear strength (Paaswell 1967;Plum and Esrig 1969;Demars and Charles 1982;Baldi et al 1988;Hueckel and Baldi 1990;Hueckel and Pellegrini 1992;Towhata et al 1993;Delage et al 2000). Uchaipichat and Khalili (2009) observed that unsaturated soils have similar volume change behavior to saturated soils when heated under normally consolidated or overconsolidated conditions.…”
Section: Temperature Effects On the Volume Change And Shear Strength Of Soilsmentioning
confidence: 99%