2015
DOI: 10.1680/jgeot.14.p.210
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Effect of pore fluid osmotic suction on matric and total suctions of compacted clay

Abstract: The experimental results of the present study on compacted expansive clay illustrate that matric suction increases with the increase in pore fluid osmotic suction due to changes in soil structure. Scanning electron micrographs show that particle stacking (aggregations) increases with increase in pore fluid osmotic suction and cation valence due to reduction in diffuse double layer thickness, and thus results in a reduction in micro pore size with a corresponding increase in macro pore size. At a given water co… Show more

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Cited by 65 publications
(33 citation statements)
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“…For the current problem under study, three distinct water retention mechanisms are considered: water adsorption, capillary retention and osmosis. The total suction (S u ) is equal to the sum of matric suction (p m ) and osmotic suction (p), according to the definition of soil suction by the International Society of Soil Science and others [23,52]. Water adsorption upon clay minerals at high suction levels and capillary retention at lower suction levels [10,48] are responsible for matric suction.…”
Section: Wrc For Mx-80 Bentonitementioning
confidence: 99%
“…For the current problem under study, three distinct water retention mechanisms are considered: water adsorption, capillary retention and osmosis. The total suction (S u ) is equal to the sum of matric suction (p m ) and osmotic suction (p), according to the definition of soil suction by the International Society of Soil Science and others [23,52]. Water adsorption upon clay minerals at high suction levels and capillary retention at lower suction levels [10,48] are responsible for matric suction.…”
Section: Wrc For Mx-80 Bentonitementioning
confidence: 99%
“…For partially saturated clays, as the salinity of water decreases and water content and clay plasticity increase, the interparticle repulsive forces increase [43]. Several researchers showed that reconstituting a clay specimen with distilled water could produce a monomodal pore size microstructure (uniform pore size) whereas aggregated microstructure (bimodal pore size) is expected as the salinity of pore water increases [5,38,44,45]. erefore, for clay specimens reconstituted at constant water content and dry density but using di erent water in terms of its salinity level, a di erent number and area of interparticle contacts are expected.…”
Section: Conceptual Understanding For the E Ect Of Pore-watermentioning
confidence: 99%
“…Table 4 shows the soil suction values in filter paper water contents ranges (w f ) <= 47% calculated by using proposed equations (Eqs. [6][7][8][9]. Figure 4 gives a linear logarithmic calibration curve for Whatman 42 filter paper used in the experimental work which is expressed by Eqs.…”
Section: Figmentioning
confidence: 99%
“…For measuring matric suction, the calibration curves are obtained from the wetting and drying of the filter papers through fluid transfer (porous plates). Total suction and pore fluid osmotic suction can be confidently determined using non-contact filter papers difference of which will give matric suction [8].…”
Section: Introductionmentioning
confidence: 99%