Advanced methods for RNA recovery from petroleum impacted soils.

Microbially-mediated hydrocarbon degradation is well documented. However, how these microbial processes occur in complex subsurface petroleum impacted systems remains unclear, and this knowledge is needed to guide technologies to enhance microbial degradation effectively. Analysis of RNA derived from soils impacted by petroleum liquids would allow for analysis of active microbial communities, and a deeper understanding of the dynamic biochemistry occurring during site remediation. However, RNA analysis in soils impacted with petroleum liquids is challenging due to: (A) RNA being inherently unstable, and (B) petroleum impacted soils containing problematic levels of polymerase chain reaction (PCR) inhibitors that must be removed to yield high-purity RNA for downstream analysis. A previously published soil wash pretreatment step and a commercially available DNA extraction kit protocol were combined and modified to be able to purify RNA from soils containing petroleum liquids.•A key modification involved reformulation of the pretreatment solution via replacing water as the diluent with a commercially-available RNA preservation solution.•Methods were developed and demonstrated using cryogenically preserved soils from three former petroleum refineries. Results showed the new soil washing approach had no adverse effects on RNA recovery but did improve RNA quality, by PCR inhibitor removal, which in turn allows for characterization of active microbial communities present in petroleum impacted soils.•In summary, our method for extracting RNA from petroleum-impacted soils provides a promising new tool for resolving metabolic processes at sites as they progress toward restoration via natural and/or engineered remediation.

Real-time soil and groundwater monitoring via spatial and temporal resolution of biogeochemical potentials.

Oxidation-reduction potentials (ORP) govern the transformation of organic compounds in water and soils. Standard methods for measurements of ORPs in subsurface setting are deeply flawed due to heterogeneous samples from wells, failure to capture weakly poised redox couples, and biases with ex-situ measurements. In this study, we developed a real-time in-situ ORP sensor system that continuously measures biogeochemical electrical potentials using vertically distributed point sensing electrodes in direct contact with the soil. Three hundred thousand data points, providing a full range of aqueous ORP values (+ 600 to - 600 mV vs. Ag/AgCl) were collected over 513 days to spatially and temporally resolve subsurface biogeochemical processes at a former petroleum refinery. Water quality and microbial community data support the validity of the ORP data. In locations impacted by petroleum light non-aqueous phase liquids (LNAPLs), barometric pumping and ebullition events drive near-daily cycles of ORP changes in the vadose zone of 400 mV. When only dissolved phase hydrocarbons are present, near-daily redox cycles are absent and values for ORP indicate methanogenic conditions immediately about the water table. When hydrocarbons are not present, redox conditions are more oxidizing by + 400 to + 700 mV. The embedded electrodes revealed variations in hydrocarbon biodegradation in time and space that cannot be resolved by collection and analysis of conventional samples of groundwater and soil gas.

Comparison of bacterial and archaeal communities in depth-resolved zones in an LNAPL body.

Advances in our understanding of the microbial ecology at sites impacted by light non-aqueous phase liquids (LNAPLs) are needed to drive development of optimized bioremediation technologies, support longevity models, and develop culture-independent molecular tools. In this study, depth-resolved characterization of geochemical parameters and microbial communities was conducted for a shallow hydrocarbon-impacted aquifer. Four distinct zones were identified based on microbial community structure and geochemical data: (i) an aerobic, low-contaminant mass zone at the top of the vadose zone; (ii) a moderate to high-contaminant mass, low-oxygen to anaerobic transition zone in the middle of the vadose zone; (iii) an anaerobic, high-contaminant mass zone spanning the bottom of the vadose zone and saturated zone; and (iv) an anaerobic, low-contaminant mass zone below the LNAPL body. Evidence suggested that hydrocarbon degradation is mediated by syntrophic fermenters and methanogens in zone III. Upward flux of methane likely contributes to promoting anaerobic conditions in zone II by limiting downward flux of oxygen as methane and oxygen fronts converge at the top of this zone. Observed sulfate gradients and microbial communities suggested that sulfate reduction and methanogenesis both contribute to hydrocarbon degradation in zone IV. Pyrosequencing revealed that Syntrophus- and Methanosaeta-related species dominate bacterial and archaeal communities, respectively, in the LNAPL body below the water table. Observed phylotypes were linked with in situ anaerobic hydrocarbon degradation in LNAPL-impacted soils.

Temperature impacts on anaerobic biotransformation of LNAPL and concurrent shifts in microbial community structure.

Thermally-enhanced bioremediation is a promising treatment approach for petroleum contamination; however, studies examining temperature effects on anaerobic biodegradation in zones containing light non-aqueous phase liquids (LNAPLs) are lacking. Herein, laboratory microcosm studies were conducted for a former refinery to evaluate LNAPL transformation, sulfate reduction, and methane generation over a one-year period for temperatures ranging from 4 to 40 °C, and microbial community shifts were characterized. Temperatures of 22 and 30 °C significantly increased total biogas generation compared to lower (4 and 9 °C) and higher temperatures (35 and 40 °C; p < 0.1). Additionally, at 22 and 30 °C methane generation commenced ~6 months earlier than for 35 and 40 °C. Statistically significant biodegradation of benzene, toluene and xylenes was observed at elevated temperatures but not at lower temperatures (p < 0.1). Additionally, a novel differential chromatogram approach was developed to overcome challenges associated with resolving losses in complex mixtures of hydrocarbons, and application of this method revealed greater losses of hydrocarbons at 22 and 30 °C as compared to lower and higher temperatures. Finally, molecular biology assays revealed that the composition and activity of microbial communities shifted in a temperature-dependent manner. Collectively, results demonstrated that anaerobic biodegradation processes can be enhanced by increasing the temperature of LNAPL-containing soils, but biodegradation does not simply increase as temperature increases likely due to a lack of microorganisms that thrive at temperatures well above the historical high temperatures for a site. Rather, optimal degradation is achieved by holding soils at the high end of, or slightly higher than, their natural range.