Chlorinated Ethene Degradation Rate Coefficients Simulated with Intact Sandstone Core Microcosms

Abiotic transformation of trichloroethene (TCE) in fractured porous rock such as sandstone is challenging to characterize and quantify. The objective of this study was to estimate the pseudo first-order abiotic reaction rate coefficients in diffusion-dominated intact core microcosms. The microcosms imitated clean flow through a fracture next to a contaminated rock matrix by exchanging uncontaminated groundwater, unamended or lactate-amended, in a chamber above a TCE-infused sandstone core. Rate coefficients were assessed using a numerical model of the microcosms that were calibrated to monitoring data. Average initial rate coefficients for complete dechlorination of TCE to acetylene, ethene, and ethane were estimated as 0.019 y(-1) in unamended microcosms and 0.024 y(-1) in lactate-amended microcosms. Moderately higher values (0.026 y(-1) for unamended and 0.035 y(-1) for lactate-amended) were obtained based on C-13 enrichment data. Abiotic transformation rate coefficients based on gas formation were decreased in unamended microcosms after similar to 25 days, to an average of 0.0008 y(-1). This was presumably due to depletion of reductive capacity (average values of 0.12 +/- 0.10 mu eeq/g iron and 18 +/- 15 mu eeq/g extractable iron). Model-derived rate coefficients and reductive capacities for the intact core microcosms aligned well with results from a previous microcosm study using crushed sandstone from the same site.