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Soil temperature is influenced by energy geo structures or any other heat sources in the ground. Ground water viscosity and density varies with thermal loading. It is expected that soil hydraulic conductivity changes with ground water density and dynamic viscosity variations. However, the effect of temperature on soil intrinsic permeability has not been completely quantified. In this research a temperature controlled permeameter cell was designed and modified to investigate any potential changes in intrinsic permeability with temperature. Experimental results determined that the thermal loading alters the soil fabric and showed reduction in intrinsic permeability with increasing temperature even for sandy soil.
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