Abstract
Vertisolic expansive soils are characterized by unique morphological features and extensive volume changes of swelling clay minerals. The engineering properties of such a soil deposit in Regina, Canada, were investigated under in situ conditions. Results indicated a bi-modal SWCC composing of a fissure AEV (10kPa) and a matrix AEV (300kPa based on water content and 6000kPa based on degree of saturation). The latter value matched the field water content and the plastic limit, of which both occurred at Save≈80%. The swell-shrink path was found to be S-shaped and included a low structural shrinkage (Save=100% to Save=80% at wp) followed by a sharp decline during normal shrinkage (Save=80% to Save=60% at ws) and then by a low decrease during residual shrinkage (Save=60% to Save=0%). An equilibrium soil microstructure for the undisturbed samples mean that for the field conditions (up to the matrix AEV), the soil aggregates remain fully saturated whereas drainage and volume changes primarily occur through the fissures.
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