Use of Bioremediation Natural Attenuation Processes for Cleanup of a TCE Groundwater Plume
The site groundwater exhibits a wide microbial diversity, with many types of aerobic and anaerobic bacteria, including the presence of low numbers of Dehalococcoides bacteria, which indicates the potential for complete reductive dechlorination of TCE and 1,1-DCE to occur at the site. In addition, key functional genes (such as TCE reductase and VC reductase) were identified at the site.
An unexpected discovery was the confirmation of a robust population of methane oxidizing bacteria (methanotrophs) which are causing the co-metabolism of TCE. Under aerobic conditions, methane oxidizing bacteria can co-metabolize or co-oxidize TCE, DCE and vinyl chloride. The presence of moderate amounts of soluble methane mono-oxygenase enzymes indicates that an increased rate of co-metabolism can be supported at this site. Based on the relative populations of methane oxidizing bacteria in comparison to DHC bacteria (up to 600 times greater), it is estimated that the co-oxidation degradation rates at the site are far greater than the reductive dechlorination rates.
Over the last four years (since 2010) of groundwater monitoring, the TCE and 1,1-DCE levels (up to 150 µg/ml) in 11 key monitoring wells have attenuated by 50% or more due to natural attenuation processes. Currently, we are in negotiation with the Los Angeles Water Quality Control Board to use natural attenuation as a 3-year strategy to obtain groundwater cleanup goals and obtain final site closure.