2014
DOI: 10.1139/cgj-2013-0089
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Soil-water characteristic curves of clays

Abstract: The drying suction – water content soil-water characteristic curves (SWCCs) of three clays (MX80 bentonite, yellow bentonite, and Speswhite kaolin) were experimentally determined using axis-translation, vapour equilibrium, and osmotic techniques. The shrinkage paths of the clays were established from Clod tests. The suction – water content SWCCs in conjunction with the Clod test results enabled establishing the suction – degree of saturation SWCCs and further determination of the air-entry values (AEVs) of the… Show more

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Cited by 73 publications
(29 citation statements)
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“…The osmotic tests results at the overlapping suction region were found to remain lower than that of water contents obtained from vapour equilibrium. Similar observation was reported by Tripathy et al [10] for other types of bentonites. The lower water contents are primarily attributed to the intrusion of PEG solution into the bentonites specimens.…”
Section: Suction-water Content Swccsupporting
confidence: 91%
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“…The osmotic tests results at the overlapping suction region were found to remain lower than that of water contents obtained from vapour equilibrium. Similar observation was reported by Tripathy et al [10] for other types of bentonites. The lower water contents are primarily attributed to the intrusion of PEG solution into the bentonites specimens.…”
Section: Suction-water Content Swccsupporting
confidence: 91%
“…The physical and microbiological properties of the Andrassy bentonite was first determined following standard laboratory procedures described in [10] [14]. The microbiological properties of the bentonite, namely bacteria and fungi determination were carried out following plating, slide culture, streaking and isolation techniques [19].…”
Section: Determination Of Geotechnical and Microbiological Propertiesmentioning
confidence: 99%
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“…Suctions obtained with the filter paper technique seem to match the psychrometer results reasonably well (see Table 1), with the biggest difference at very high suction where filter paper measurements are known to be less reliable. Furthermore, it is expected that, on average, the difference between total and matric suction in case of samples saturated with deionised water should be low (as the osmotic suction component should be zero assuming no salt is present in the natural bentonite; very small amounts of salt may be present though [20]). That is indeed confirmed -the average difference between the matric and total suction measurements (for all the samples partially saturated with water) is just 0.083 MPa.…”
Section: Accuracy Of the Resultsmentioning
confidence: 99%
“…It is anticipated that changes in the pore fluid ionic concentrations would affect the engineering behavior of soils [22][23] [24]. Estabragh et al [25] noted that the magnitude of soil deformation is affected by the water quality.…”
Section: Compressibility Behaviormentioning
confidence: 99%