Tracer diffusion coefficients in sedimentary rocks: Correlation to porosity and hydraulic conductivity
Date of Original Version
Matrix diffusion is an important transport process in geologic materials of low hydraulic conductivity. For predicting the fate and transport of contaminants, a detailed understanding of the diffusion processes in natural porous media is essential. In this study, diffusive tracer transport (iodide) was investigated in a variety of geologically different limestone and sandstone rocks. Porosity, structural and mineralogical composition, hydraulic conductivity, and other rock properties were determined. The effective diffusion coefficients were measured using the time-lag method. The results of the diffusion experiments indicate that there is a close relationship between total porosity and the effective diffusion coefficient of a rock (analogous to Archie's Law). Consequently, the tortousity factor can be expressed as a function of total porosity. The relationship fits best for thicker samples (>1.0 cm) with high porosities (>20%), because of the reduced influence of heterogeneity in larger samples. In general, these correlations appear to be a simple way to determine tortuosity and the effective diffusion coefficient from easy to determine rock porosity values. Copyright © 2001 Elsevier Science B.V.
Journal of Contaminant Hydrology
Boving, Thomas B., and Peter Grathwohl. "Tracer diffusion coefficients in sedimentary rocks: Correlation to porosity and hydraulic conductivity." Journal of Contaminant Hydrology 53, 1-2 (2001): 85-100. doi:10.1016/S0169-7722(01)00138-3.