SCI和EI收录∣中国化工学会会刊

Chinese Journal of Chemical Engineering ›› 2024, Vol. 71 ›› Issue (7): 122-131.DOI: 10.1016/j.cjche.2024.02.012

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Study on the evolution of solid–liquid–gas in multi-scale pore methane in tectonic coal

Junjie Cai1, Xijian Li1,2, Hao Sui1, Honggao Xie2   

  1. 1. College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China;
    2. Mining College, Guizhou University, Guiyang 550025, China
  • Received:2023-12-09 Revised:2024-02-02 Online:2024-08-30 Published:2024-07-28
  • Contact: Xijian Li,E-mail:xjli1@gzu.edu.cn
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (52164015), the Technology Funding Projects of Guizhou Province ([2022]231).

Study on the evolution of solid–liquid–gas in multi-scale pore methane in tectonic coal

Junjie Cai1, Xijian Li1,2, Hao Sui1, Honggao Xie2   

  1. 1. College of Resources and Environmental Engineering, Guizhou University, Guiyang 550025, China;
    2. Mining College, Guizhou University, Guiyang 550025, China
  • 通讯作者: Xijian Li,E-mail:xjli1@gzu.edu.cn
  • 基金资助:
    This work was supported by the National Natural Science Foundation of China (52164015), the Technology Funding Projects of Guizhou Province ([2022]231).

Abstract: The rich accumulation of methane (CH4) in tectonic coal layers poses a significant obstacle to the safe and efficient extraction of coal seams and coalbed methane. Tectonic coal samples from three geologically complex regions were selected, and the main results obtained by using a variety of research tools, such as physical tests, theoretical analyses, and numerical simulations, are as follows: 22.4–62.5 nm is the joint segment of pore volume, and 26.7–100.7 nm is the joint segment of pore specific surface area. In the dynamic gas production process of tectonic coal pore structure, the adsorption method of methane molecules is “solid–liquid adsorption is the mainstay, and solid–gas adsorption coexists”. Methane stored in micropores with a pore size smaller than the jointed range is defined as solid-state pores. Pores within the jointed range, which transition from micropore filling to surface adsorption, are defined as gaseous pores. Pores outside the jointed range, where solid–liquid adsorption occurs, are defined as liquid pores. The evolution of pore structure affects the methane adsorption mode, which provides basic theoretical guidance for the development of coal seam resources.

Key words: Tectonic coal, Multiscale pore structure, Methane adsorption, Micropore filling, Monolayer, Molecular simulation

摘要: The rich accumulation of methane (CH4) in tectonic coal layers poses a significant obstacle to the safe and efficient extraction of coal seams and coalbed methane. Tectonic coal samples from three geologically complex regions were selected, and the main results obtained by using a variety of research tools, such as physical tests, theoretical analyses, and numerical simulations, are as follows: 22.4–62.5 nm is the joint segment of pore volume, and 26.7–100.7 nm is the joint segment of pore specific surface area. In the dynamic gas production process of tectonic coal pore structure, the adsorption method of methane molecules is “solid–liquid adsorption is the mainstay, and solid–gas adsorption coexists”. Methane stored in micropores with a pore size smaller than the jointed range is defined as solid-state pores. Pores within the jointed range, which transition from micropore filling to surface adsorption, are defined as gaseous pores. Pores outside the jointed range, where solid–liquid adsorption occurs, are defined as liquid pores. The evolution of pore structure affects the methane adsorption mode, which provides basic theoretical guidance for the development of coal seam resources.

关键词: Tectonic coal, Multiscale pore structure, Methane adsorption, Micropore filling, Monolayer, Molecular simulation