Abstract
A facies-based approach was used to delineate both geochemical and physical aquifer property heterogeneity. Specifically, the parameters considered were the sorption coefficient (K(d)) for a model organic contaminant and hydraulic conductivity (K) inferred from the particle size distribution. Subfacies-sized samples were analyzed for both tetrachloroethene K(d) and K in a vertical core of the Borden aquifer. Both parameters were correlated with the six sedimentary facies identified within the vertical core. As a consequence of their relations to sedimentary facies, significant positive correlations between In K and In K(d) which were different from the core-scale correlation and different from each other were identified for some facies. Facies-specific correlations generally resulted in improved statistics (i.e., higher correlation coefficients and reduced confidence intervals) compared to the core-scale correlation. The results suggest that a facies-based approach can be useful in characterizing the heterogeneity of the transport properties of sedimentary aquifers.
| Original language | English |
|---|---|
| Pages (from-to) | 385-396 |
| Number of pages | 12 |
| Journal | Water Resources Research |
| Volume | 34 |
| Issue number | 3 |
| DOIs | |
| State | Published - Mar 1998 |
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