2005
DOI: 10.1061/(asce)1090-0241(2005)131:5(654)
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Nature of Soil–Water Characteristic Curve for Plastic Soils

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Cited by 61 publications
(34 citation statements)
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“…It is noted that this tendency exists for both total and matric suction, however, for the total suction, this correlation has a higher value of R 2 (0.71). It is interesting to analyze the difference (D) in suction in relation to soil plasticity because plasticity can provide an approximate estimation of soil suction [8]. Fig.3 presents the obtained results in terms of the maximum difference (D) against the liquid limit (LL) of soil.…”
Section: Resultsmentioning
confidence: 99%
“…It is noted that this tendency exists for both total and matric suction, however, for the total suction, this correlation has a higher value of R 2 (0.71). It is interesting to analyze the difference (D) in suction in relation to soil plasticity because plasticity can provide an approximate estimation of soil suction [8]. Fig.3 presents the obtained results in terms of the maximum difference (D) against the liquid limit (LL) of soil.…”
Section: Resultsmentioning
confidence: 99%
“…The soil-water characteristic curve for the Malda soil is determined by following the standard test method [2,25] using tensiometers. The soil was first dried and then known amount of water is added to it.…”
Section: Soil-water Characteristics Curve (Swcc)mentioning
confidence: 99%
“…The rainfall intensities considered in this study are 2,4,8,16,25, and 32 mm/h. For each case, the rainfall infiltration rate is computed from the rainfall intensity and the duration of the rainfall, and applied as a boundary flux across the slope.…”
Section: Water Table Fluctuation and Reduction Of Suction Pressure Wimentioning
confidence: 99%
“…Beyond this air entry into the pore space, the soil suction is steadily increasing, with reducing volumetric water content. In the case of extremely high soil suction, the volumetric water content approaches a residual water content, θ R , at which water is not further drained out and is held in the soil matrix by adsorptive forces to the particle surface [61]. In contrast to the IDC, the IWC starts at dry condition, with water content close to zero.…”
Section: Swccmentioning
confidence: 99%
“…At soil-water phase state equilibrium, hydraulic stress is described by negative pore water pressure [77,80]. For instance, volume reduction occurs under soil desiccation due to the suction-induced capillary forces [26,51,61,81]. The capillary rise of water during desiccation implies a contractile force exerted by the curved meniscus at the interface of the air and water phase [82].…”
Section: External Stress and Internal Stressmentioning
confidence: 99%