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• W2014080719 abstract "Both hydrologic and thermal transport properties play a significant role in the movement of heat through permeable sedimentary material; however, the thermal conductivity is rarely characterized in detailed spatial resolution. As part of a study of the movement of thermal plumes through a sand and gravel aquifer, we have constructed a two‐dimensional profile of thermal conductivity. This work consisted of: (i) measuring the thermal conductivity of the soil solids, λ s , for the main stratigraphic units using the steady‐state divided‐bar apparatus and estimating conductivity from mineral composition; (ii) measuring the volumetric water content and porosity using crosshole ground‐penetrating radar; (iii) evaluating four models used to predict the apparent thermal conductivity, λ, of variably saturated soils and selecting the best model using the information‐theoretic approach, (iv) calculating the λ field on a 0.25‐m square cell grid using measured data and the selected model, and (v) simulating thermal transport within the two‐dimensional domain using a finite element numerical model. The apparent thermal conductivity in the saturated aquifer ranges from 2.14 to 2.69 W m −1 K −1 with a mean of 2.42 W m −1 K −1 Numerical simulations show that the heterogeneous thermal conductivity field results in increased thermal dispersion that is most pronounced at the plume front. Our values for λ and λ s may be used for glacial soils with similar mineralogy and texture. Our methods may also be used at other sites to construct the thermal conductivity distribution." @default.
• W2014080719 created "2016-06-24" @default.
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• W2014080719 creator A5045785163 @default.
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• W2014080719 date "2006-07-01" @default.
• W2014080719 modified "2023-10-03" @default.
• W2014080719 title "Characterizing the Two‐Dimensional Thermal Conductivity Distribution in a Sand and Gravel Aquifer" @default.
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• W2014080719 doi "https://doi.org/10.2136/sssaj2005.0293" @default.
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