1983
DOI: 10.1016/0148-9062(83)91683-2
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Mechanisms controlling the secondary compression of clays

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Cited by 5 publications
(7 citation statements)
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“…Therefore, the increase in the LL of RM/TCE mixture cannot be explained by variations in the density-viscosity of the pore fluid, but likely is related with the strong decrease in e that enhances inter-particle attractive forces and aggregation of RM, as evidenced by SEM (Fig. 2), thus increasing its shearing resistance and the LL, in a similar manner to as described for kaolinite (Sridharan and Rao 1975). In contrast to pure organics, neither heptane-nor TCE-saturated aqueous solutions changed Atterberg limits of the RM (Table 4).…”
Section: Atterberg Limitsmentioning
confidence: 60%
“…Therefore, the increase in the LL of RM/TCE mixture cannot be explained by variations in the density-viscosity of the pore fluid, but likely is related with the strong decrease in e that enhances inter-particle attractive forces and aggregation of RM, as evidenced by SEM (Fig. 2), thus increasing its shearing resistance and the LL, in a similar manner to as described for kaolinite (Sridharan and Rao 1975). In contrast to pure organics, neither heptane-nor TCE-saturated aqueous solutions changed Atterberg limits of the RM (Table 4).…”
Section: Atterberg Limitsmentioning
confidence: 60%
“…It has been reported that w L increases marginally with increasing concentration of ions in the pore water. Increasing the concentration and the valence of the ions in the pore fluid causes coagulation of the minerals, which leads to a higher liquid limit (Horpibulsuk et al 2011;Sridharan and Venkatappa Rao 1975;Sridharan et al 1986Sridharan et al , 1988.…”
Section: Kaolinite Mineralsmentioning
confidence: 99%
“…NaCl in saline waters causes the thickness of the diffuse double layer to shrink, limiting the volume change behaviour (Thøgersen 2001;Sridharan and Venkatappa Rao 1973). Thus, the w L decreases with an increase of salinity for smectite-rich clays (Horpibulsuk et al 2011;Sridharan and Venkatappa Rao 1975;Sridharan et al 1986Sridharan et al , 1988. The liquid limit, plastic limit, undrained shear strength and deformation potential, etc.…”
Section: Diffuse Double Layers Of Clay Particlesmentioning
confidence: 99%
“…Due to intrinsic factors that characterize the viscous behavior to the creep of the structure clay in the secondary stage, there is still no complete understanding of the underlying mechanisms to this phenomenon. However, Sridharan and Rao [38] suggested that secondary compression is related to the delayed deformation of the clay particle after the raw water is drained from the pores in the primary structure (see also Hueckel [39]). This secondary deformation arises from some due to the delayed drainage of the adsorbed water concerning the flow of the bulk phase.…”
Section: Introductionmentioning
confidence: 99%