Swelling Characteristics and Interaction Mechanism of High-Rank Coal during CO₂ Injection: A Molecular Simulation Study

Abstract

In CO 2 -enhanced coalbed methane (CO 2 -ECBM) engineering, accurate knowledge of the interaction mechanism of CO 2 and coal matrix is crucial for improving the recovery of CH 4 and contributing to the geological sequestration of CO 2 . This study is performed to prove the accuracy of molecular simulation and calculate the variation characteristics of pore structure, volumetric strain, mechanical properties, Fourier transform infrared (FT-IR) spectra, and the system free energy by molecular dynamics (MD) and grand canonical Monte Carlo (GCMC) methods. According to the obtained results, a relationship between pore structure, swelling strain, mechanical properties, chemical structure, and surface free energy was established. Then, the correlation of various coal change characteristics was analyzed to elucidate the interaction mechanism between CO 2 and coal. The results showed that (1) the molecular simulation method was able to estimate the swelling mechanism of CO 2 and coal. However, because the adsorption capacity of the molecular simulate is greater than that of the experiment and the raw coal is softer than the macromolecular structure, the molecular results are slightly better than the experimental results. (2) As pressure increased from 0 to 4 MPa, the intramolecular pores and sorption-induced strain changed significantly, whereas when the pressure increased from 4 to 8 MPa (especially at 6–8 Mpa), there was an increase of the intermolecular pores and mechanical properties and transition from elastic to plastic. In addition, when the pressure was >8 MPa, the coal matrix changed slightly. ScCO 2 with a higher adsorption capacity results in greater damage and causes larger alterations of coal mechanical properties. (3) The change of the coal matrix is essentially controlled by the surface free energy of the molecular system. E valence affects the aromatic structure and changes the volume of the intramolecular pores, thus affecting the sorption-induced strain change rate. E non affects the length of side chains and the disorder degree of coal molecules and changes the volume of the intramolecular pores, thus affecting the mechanical property change rate. Our findings shed light on the dynamic process of coal swelling and provide a theoretical basis for CO 2 enhancing the recovery of CH 4 gas in coal.

Molecular Simulation of the Pore Structure and Adsorption Properties of Coal under Compression Stress

“…18,19 Many studies have shown that stress can not only change the macroscopic physical structure of coal but also cause rearrangement of the macromolecular structure of coal. 20,21 The macromolecule of coal is characterized by a high degree of complexity and heterogeneity, and it is composed of a series of aromatic hydrocarbons with different degrees of condensation, a large number of aliphatic side chains, and oxygen-containing functional groups. 22 only affects the fringe length, tortuosity, and fringe separation distributions, 23,24 but also changes the structure and distribution of aliphatic side chains and functional groups.…”

“…The shape of the pores also has a different effect on adsorption; the adsorption capacity of cylindrical pores is higher than that of spherical pores . Researchers also found that the ultra micropores (smaller than 1 nm) are associated with the macromolecular structure of coal. , Many studies have shown that stress can not only change the macroscopic physical structure of coal but also cause rearrangement of the macromolecular structure of coal. , The macromolecule of coal is characterized by a high degree of complexity and heterogeneity, and it is composed of a series of aromatic hydrocarbons with different degrees of condensation, a large number of aliphatic side chains, and oxygen-containing functional groups . Tectonic stress not only affects the fringe length, tortuosity, and fringe separation distributions, , but also changes the structure and distribution of aliphatic side chains and functional groups. , An increase in ground stress causes a decrease in the average interlayer spacing and reduces the pore volume of the coal .…”