4.6 Article

Links of Hydrogen Sulfide Content With Fluid Components and Physical Properties of Carbonate Gas Reservoirs: A Case Study of the Right Bank of Amu Darya, Turkmenistan

Journal

FRONTIERS IN EARTH SCIENCE
Volume 10, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/feart.2022.910666

Keywords

carbonate gas reservoir; hydrogen sulfide; heavy hydrocarbon; TSR; fracture

Funding

  1. Scientific Research and Technology Development Project of CNPC [2021DJ3301]
  2. General Special Scientific Research Plan of the Shaanxi Provincial Department of Education [20JK0848]

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This study provides a comprehensive analysis of the links between hydrogen sulfide (H2S) content and fluid components as well as petrophysical properties in carbonate gas reservoirs. The results show that H2S content is strongly correlated with fluid components and has a significant impact on porosity and permeability of the reservoir. The study also identifies sulfate thermochemical reduction (TSR) as the dominant contributor to high H2S content in carbonate reservoirs. Pore volume enlargement and the dissolution effect of acidic gases are found to be the main mechanisms for TSR to improve carbonate reservoir properties.
Hydrogen sulfide (H2S) in carbonate gas reservoirs shows strong relevance with the natural gas components and has an obvious impact on reservoir types and their petrophysical properties. In this work, core and fluid samples were collected from the Right Bank of Amu Darya reservoirs, Turkmenistan. Then, fluid composition analysis and flash evaporation experiments were performed to investigate the components of reservoir fluid. Petrophysical properties, that is, porosity and permeability, and micropore structures of cores were determined by permeameter-porosimeter and scanning electron microscope (SEM) analysis, respectively. Results in this work indicate that the H2S content shows obvious relevance to fluid components in carbonate gas reservoirs. With the increase of H2S content, the total heavy hydrocarbons and potential condensate content decrease, while the condensate density increases. In addition, at higher H2S content, larger pore and vug porosity was observed. However, in reservoirs with lower H2S content, the matrix pores are relatively tight and prone to develop fractures. Furthermore, sulfate thermochemical reduction (TSR) is found to be the dominant contributor to high H2S content in carbonate reservoirs through material and thermodynamic condition analysis. The Gibbs free energy and normalized hydrocarbon content show that the consumption of heavy hydrocarbons generally increases with carbon numbers during TSR, but reaches a minimum at the components of C-7 to C-9. Finally, the relationship between TSR and rock petrophysical properties was discussed, indicating that pore volume enlargement and the dissolution effect of acidic gases are the main mechanisms for TSR to improve carbonate reservoir property. Results in this study present comprehensive analyses of the links between H2S content and fluid components and petrophysical properties in carbonate gas reservoirs.

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