Oil & Gas Geology ›› 2025, Vol. 46 ›› Issue (1): 304-314.doi: 10.11743/ogg20250121

• Methods and Technologies • Previous Articles     Next Articles

Molecular simulations of a multicomponent hydrocarbon-water mixture in the organic matter-clay mineral composite pore system of lacustrine shales: A case study of the Da’anzhai Member of the Jurassic Ziliujing Formation, Sichuan Basin

Wenxi REN1(), Xiaojun ZENG1, Guangfu WANG2, Jianchun GUO1, Yuxuan LIU1   

  1. 1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Southwest Petroleum University,Chengdu,Sichuan 610500,China
    2.Petroleum Exploration and Production Research Institute,SINOPEC,Beijing 102206,China
  • Received:2024-06-21 Revised:2024-11-06 Online:2025-02-28 Published:2025-03-03

Abstract:

Given the diverse hydrocarbon compositions of the Jurassic lacustrine shale gas in the Sichuan Basin, we develop a molecular model for the organic matter-clay mineral composite pore system composed of kerogen and illite slit pores and composite pores. Using molecular dynamics simulations, we explore the microscopic occurrence characteristics of wet gas in the composite pore system and the influential factors related. The results indicate that at lower pressures, hydrocarbon molecules preferentially occupy space near kerogen walls within the composite pores, while the number of hydrocarbon molecules increases under high-pressure conditions, and the heavier hydrocarbon molecules are preferentially concentrated in space near kerogen walls within the composite pores, leaving lighter hydrocarbons to be confined to the illite walls. Under the same pressure conditions, a larger pore diameter meaning larger pore space, can accommodate more hydrocarbon molecules. Under high-pressure conditions, interactions between water molecules get enhanced, forming clusters due to hydrogen bonding. These water clusters can be found on the surface of the kerogen, or free in the composite pores, or develop into a water film on the surface of illite. The organic matter pores, composite pores, and clay mineral pores in the organic matter-clay mineral composite pore system all contribute to the occurrence of hydrocarbons. Compared to organic matter pores, the latter two pore types can accommodate a greater number of hydrocarbon molecules dominated by lighter ones, characterized by higher gas content and better mobility.

Key words: kerogen, illite, wet gas, molecular simulation, composite pore system, lacustrine shale gas, Sichuan Basin

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