The origins of volatile organic sulfur compounds in natural gas reservoirs

Abstract

<p>Volatile organic sulfur compounds (VOSC) are known to occur in natural gas and petroleum reservoirs. These compounds are typically accompanied by H<sub>2</sub>S which together, degrade the quality of the petroleum, complicate production due to corrosion of piping, and pose a health risk to workers and local communities. The origins of both H<sub>2</sub>S and VOSC in natural gas are only partially understood with the latter being analyzed in only a few cases and its formation processes virtually unknown. Nevertheless, several studies have linked VOSC to H<sub>2</sub>S in processes such as thermochemical sulfate reduction (TSR) and kerogen cracking. Hence, VOSC have the potential to act as a proxy for the natural gas and H<sub>2</sub>S origins, in-situ TSR and fluid migration pathways.</p><p>To better understand the pathways of VOSC formation in natural gas reservoirs, we analyzed natural gas samples (Permian reservoirs, Sichuan Basin, China) and performed a series of pyrolysis experiments. The results of the experiments between methane (CH<sub>4</sub>) and H<sub>2</sub>S at 360°C for 4-96 hours revealed the only VOSC formed is methanethiol (MeSH) which was identified at ppm concentrations in all experiments. The δ<sup>34</sup>S values of the MeSH were 2 to 3‰ heavier than the initial H<sub>2</sub>S. For comparison, Meshoulam et al., (2021) reported that the reaction between H<sub>2</sub>S and pentane (i.e. “wet gas”) that yielded a variety of VOSCs from thiols to methyl-thiophenes in the gas phase and up to methyl-benzothiophenes in the liquid phase. The analysis of natural gases showed that the samples contain a large variety of thiols and sulfides. The diversity of VOSC identified carries some resemblance to that observed by Meshoulam et al., (2021) and may suggest these VOSC are the result of in-reservoir reaction of C<sub>2</sub>+ hydrocarbons with H<sub>2</sub>S. The analysis of δ<sup>34</sup>S values of the VOSCs showed they cover a range between +10 to +30‰ while most samples had their VOSC in a narrower range of approximately 8‰. Generally, samples show a positive correlation between H<sub>2</sub>S content and VOSCs concentration- thereby implying VOSCs formation in the gas-phase. The δ<sup>34</sup>S of thiols in five of the samples covered a narrower isotopic range of about 2‰ while the sulfides in the samples spread over a large isotopic range of up to 10‰. This observation suggests the thiols are in isotopic equilibrium with their associated H<sub>2</sub>S while the sulfides are not. The reason for this difference is unclear. Further analysis will shed more light on isotopic fractionations between VOSC and H<sub>2</sub>S and will thus allow identification of H<sub>2</sub>S origins in the studied area.</p><p>[1] Meshoulam, A., Said-Ahmad, W., Turich, C., Luu, N., Jacksier, T., Shurki, A., Amrani, A., 2021. Experimental and theoretical study on the formation of volatile sulfur compounds under gas reservoir conditions. <em>Organic Geochemistry</em>, 152, 104175</p>