2017
DOI: 10.1680/jgere.17.00002
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Behaviour of MH silts with varying plasticity indices

Abstract: It is important for geotechnical engineers to understand the intrinsic and mechanical behaviour of silt as it is presently recognised that there exist gaps in understanding its fundamental behaviour. The behaviour of kaolin samples with varying clay and silt contents was investigated in the present study. This study characterised the samples by their corresponding ranges of plasticity index (P I ) -namely, P I £ 13% and P I > 13%. This outcome is achieved by interpreting the results of Atterberg limit tests, p… Show more

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Cited by 23 publications
(11 citation statements)
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“…Atterberg limits are considered a fundamental concept of soil consistency in soil classification. Atterberg limit tests define the boundaries where clay and silt go through four different physical changes (solid, semi-solid, plastic, and liquid) by moisture content variation [172]. Figure 10 demonstrates how different biopolymers can affect the Atterberg limits of soils.…”
Section: Atterberg Limitsmentioning
confidence: 99%
“…Atterberg limits are considered a fundamental concept of soil consistency in soil classification. Atterberg limit tests define the boundaries where clay and silt go through four different physical changes (solid, semi-solid, plastic, and liquid) by moisture content variation [172]. Figure 10 demonstrates how different biopolymers can affect the Atterberg limits of soils.…”
Section: Atterberg Limitsmentioning
confidence: 99%
“…However, the difference of compressibility for isotropic and K 0 consolidations was higher for higher preconsolidation e. Similarly, the loose (DE-CIU24 and DE-K 0 U04) and dense (DE-CIU21 and DE-K 0 U03) pairs from DEM simulations showed different compressibilities for different consolidation paths. The K 0 consolidation paths showed slightly higher compression than isotropic consolidation, which increases with e. The purpose of Figure 4 is not to compare quantitatively the results from experiments and DEM simulations, but to capture the change in compressibility for isotropic and K 0 consolidations and the trend of increasing compressibility with e for YS sand and other experimental studies (Butterfield and Marchi, 2017;Wong et al, 2017). Figure 4(b) shows the stress ratio (K ¼ s 0 3 =s 0 1 ) evolution paths of the triaxial tests and DEM simulations (presented in Figure 4(a)) in the K −s 0 1 space.…”
Section: Controlling Module In Dem Simulationmentioning
confidence: 99%
“…For example, the friction angle, stiffness, and permeability decrease with increased clay percentage, while these parameters increase with increased sand content. The behaviour of soils with a higher percentage of clay particles shows more stress softening behaviour, while the soils with a higher percentage of sand particles show more stress hardening behaviour [35,36].…”
Section: Introductionmentioning
confidence: 99%