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地层条件下元素硫在硫化氢中溶解的分子机制。

Molecular mechanism of elemental sulfur dissolution in HS under stratal conditions.

作者信息

Yuan Sheng, Wan Ying, Wang Li, Li Nong, Yang Mingli, Yu Shengping, Zhang Li

机构信息

Institute of Atomic and Molecular Physics, Sichuan University Chengdu 610065 China

Research Institute of Exploration and Development, PetroChina Southwest Oil and Gasfield Company Chengdu 610213 China.

出版信息

RSC Adv. 2024 May 28;14(24):17184-17194. doi: 10.1039/d4ra01764a. eCollection 2024 May 22.

Abstract

Resulting from the solubility reduction of elemental sulfur during the development of high sulfur gas formations, sulfur deposition often occurs to reduce the gas production and threaten the safety of gas wells. Understanding the dissolution mechanism of elemental sulfur in natural gas is essential to reduce the risk caused by sulfur deposition. Because of the harsh conditions in the high-sulfur formations, it remains challenging to characterize the dissolution-precipitation processes, making deficient the knowledge of sulfur dissolution mechanism. The dissolution of sulfur allotropes (S, = 2, 4, 6 and 8) in HS, the main solvent of sulfur in natural gas, is studied in this work by means of first-principles calculations and molecular dynamics simulations. While S and S undergo physical interaction with HS under the conditions corresponding to those at 1-6 km stratigraphic depths, S and S react with HS and form stable polysulfides. Unravelling the mechanism would be helpful for understanding and controlling the sulfur deposition in high-sulfur gas development.

摘要

在高含硫气藏开发过程中,由于单质硫溶解度降低,常发生硫沉积,从而降低气产量并威胁气井安全。了解单质硫在天然气中的溶解机制对于降低硫沉积带来的风险至关重要。由于高含硫地层条件苛刻,表征溶解 - 沉淀过程仍具有挑战性,导致对硫溶解机制的认识不足。本工作通过第一性原理计算和分子动力学模拟研究了硫的同素异形体(S₂、S₄、S₆和S₈)在天然气中硫的主要溶剂H₂S中的溶解情况。在对应于地层深度1 - 6千米的条件下,S₂和S₄与H₂S发生物理相互作用,而S₆和S₈与H₂S反应并形成稳定的多硫化物。揭示该机制将有助于理解和控制高含硫气藏开发中的硫沉积。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd07/11131937/ba2020e43194/d4ra01764a-f1.jpg

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