Bioaugmentation of butane-utilizing microorganisms to promote cometabolismof 1,1,1-trichloroethane in groundwater microcosms

The transformation of 1,1,1-trichloroethane (1,1,1-TCA) in ioaugmented and non-augmented microcosms was evaluated. The microcosms contained roundwater and aquifer materials from a test site at Moffett Field, Sunnyvale, CA. Th e initial inoculum for bioaugmentation was a butane-utilizing enrichment fr om the subsurface of the Hanford DOE site. The non-augmented microcosm requ ired 80 days of incubation before butane-utilization was observed while the augmented microcosms required 3 days. Initially the augmented microcosms w ere effective in transforming 1,1,1-TCA, but their transformation ability d ecreased after prolonged incubation. The non-augmented microcosms initially showed limited 1,1,1-TCA transformation but improved with time. After 440 days, both the non-augmented and augmented microcosms had similar transform ation yields (0.04 mg 1,1,1-TCA/mg butane) and had similar microbial compos ition (DNA fingerprints). Subsequent microcosms, when bioaugmented with a H anford enrichment that was repeatedly grown in 100% mineral media, did not effectively grow or transform 1,1,1-TCA under groundwater nutrient conditio ns. Microcosm tests to study the effect of mineral media on transformation ability were performed with the Hanford enrichment. Microcosms with 50% min eral media in groundwater most effectively utilized butane and transformed 1,1,1-TCA, while microcosms with groundwater only and microcosms with 5% mi neral media in groundwater lost their 1,1,1-TCA transformation ability. DNA fingerprinting indicated shifts in the microbial composition with the diff erent mineral media combinations. Successful bioaugmentation was achieved b y enriching butane-utilizers from Moffett Field microcosms that were effect ive in groundwater with no mineral media added. The results suggest that su ccessful in-situ bioaugmentation might be achieved through the addition of enriched cultures that perform well under subsurface nutrient conditions.