Abstract

Hydraulic fracturing of black shale formations has greatly increased United States oil and natural gas recovery. However, the accumulation of biomass in subsurface reservoirs and pipelines is detrimental because of possible well souring, microbially induced corrosion, and pore clogging. Temporal sampling of produced fluids from a well in the Utica Shale revealed the dominance of Halanaerobium strains within the in situ microbial community and the potential for these microorganisms to catalyze thiosulfate-dependent sulfidogenesis. From these field data, we investigated biogenic sulfide production catalyzed by a Halanaerobium strain isolated from the produced fluids using proteogenomics and laboratory growth experiments. Analysis of Halanaerobium isolate genomes and reconstructed genomes from metagenomic data sets revealed the conserved presence of rhodanese-like proteins and anaerobic sulfite reductase complexes capable of converting thiosulfate to sulfide. Shotgun proteomics measurements using a Halanaerobium isolate verified that these proteins were more abundant when thiosulfate was present in the growth medium, and culture-based assays identified thiosulfate-dependent sulfide production by the same isolate. Increased production of sulfide and organic acids during the stationary growth phase suggests that fermentative Halanaerobium uses thiosulfate to remove excess reductant. These findings emphasize the potential detrimental effects that could arise from thiosulfate-reducing microorganisms in hydraulically fractured shales, which are undetected by current industry-wide corrosion diagnostics. IMPORTANCE Although thousands of wells in deep shale formations across the United States have been hydraulically fractured for oil and gas recovery, the impact of microbial metabolism within these environments is poorly understood. Our research demonstrates that dominant microbial populations in these subsurface ecosystems contain the conserved capacity for the reduction of thiosulfate to sulfide and that this process is likely occurring in the environment. Sulfide generation (also known as "souring") is considered deleterious in the oil and gas industry because of both toxicity issues and impacts on corrosion of the subsurface infrastructure. Critically, the capacity for sulfide generation via reduction of sulfate was not detected in our data sets. Given that current industry wellhead tests for sulfidogenesis target canonical sulfate-reducing microorganisms, these data suggest that new approaches to the detection of sulfide-producing microorganisms may be necessary.

Highlights

  • Hydraulic fracturing of black shale formations has greatly increased United States oil and natural gas recovery

  • Thiosulfate was initially present at lower concentrations (~2 mg/liter) in produced waters and was likely derived from both hydraulic fracturing chemical additives and the leaching of salts from shale during water-rock interactions [15] (Fig. S2)

  • Because of concerns associated with sulfidogenesis and scale formation, input waters rich in oxidized sulfur species are typically not used in hydraulic fracturing processes

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Summary

Introduction

Hydraulic fracturing of black shale formations has greatly increased United States oil and natural gas recovery. Despite the application of biocides during the hydraulic fracturing process, a series of studies have revealed that microorganisms colonize these newly fractured shales and persist over extended periods of time (Ͼ300 days) [3,4,5,6] Such biomass accumulations in pipelines and reservoirs may be detrimental because of the potential for souring (production of H2S), microbially induced corrosion, and pore clogging by cells and biogenic gases [7, 8]. Geochemical measurements of produced fluids from this site identified the presence of thiosulfate, while sulfur isotope measurements of the same samples were diagnostic of microbial reduction of oxidized sulfur compounds These findings suggest that current industry monitoring centered on sulfate-mediated sulfidogenesis would not account for Halanaerobium sulfide generation, with long-term ramifications in hydraulically fractured environments

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