<p>Storage of multiphase and multicomponent fluids in coal is crucial for accurate reserve estimation and effective exploration. A macromolecular model of anthracite was built, and adsorptions of pure gas and gas mixture of CO<sub>2</sub> and CH<sub>4</sub> under a series of low temperatures (233.15–313.15 °K), pressures (0–30&#xa0;MPa) and water content (0–2.74%) conditions were simulated. The absolute adsorption of each component increased with pressure and its molar fraction decreased with increase in temperature and water content. CO<sub>2</sub> had a larger adsorption capacity, isosteric heat and interaction energies compared with CH<sub>4</sub> due to its smaller size and quadrupole moment. The interaction energy was positively related to the adsorption amount. The adsorption selectivity of CO<sub>2</sub> over CH<sub>4</sub> decreased with increase in CO<sub>2</sub> partial pressure and temperature, while it increased with water content due to a significant reduction in the accessible volume for CH<sub>4</sub>. The adsorbate distribution peaks on the N- and O-functional groups reduced while those on the S-functional group increased with increase in water content. The density of CH<sub>4</sub> decreased significantly with increase in CO<sub>2</sub> molar fraction, and its distribution area was smaller than that of CO<sub>2</sub>.</p>

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Molecular Study on Storage of CO2 and CH4 in Anthracite with Different Water Content Under Liquid CO2-ECBM Circumstances

  • Decheng Zhang,
  • Junjie Wan,
  • Guanglei Zhang,
  • Tianshou Ma,
  • Yi Ding,
  • Wen Nie,
  • P. G. Ranjith,
  • M. S. A. Perera,
  • Beining Zhang

摘要

Storage of multiphase and multicomponent fluids in coal is crucial for accurate reserve estimation and effective exploration. A macromolecular model of anthracite was built, and adsorptions of pure gas and gas mixture of CO2 and CH4 under a series of low temperatures (233.15–313.15 °K), pressures (0–30 MPa) and water content (0–2.74%) conditions were simulated. The absolute adsorption of each component increased with pressure and its molar fraction decreased with increase in temperature and water content. CO2 had a larger adsorption capacity, isosteric heat and interaction energies compared with CH4 due to its smaller size and quadrupole moment. The interaction energy was positively related to the adsorption amount. The adsorption selectivity of CO2 over CH4 decreased with increase in CO2 partial pressure and temperature, while it increased with water content due to a significant reduction in the accessible volume for CH4. The adsorbate distribution peaks on the N- and O-functional groups reduced while those on the S-functional group increased with increase in water content. The density of CH4 decreased significantly with increase in CO2 molar fraction, and its distribution area was smaller than that of CO2.