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This study investigates the osmotic flow and hydraulic conductivity of undisturbed Cretaceous clay samples from southern Saskatchewan, demonstrating that clays can act as semipermeable membranes affecting groundwater flow and solute transport. Laboratory experiments revealed that the hydraulic conductivity of the clay increased with pore-fluid concentration, while osmotic efficiencies varied significantly. The findings highlight the importance of osmotic behavior in low hydraulic conductivity aquitards and

Author

ridec400

Language

EN