Effects of CO2 on the Micron-scale Pore-fracture Structure and Connectivity in Coals from the Qinshui Basin

DOI:10.14800/IOGR.1189

Abstract

The changes in the micron-scale pore and fracture structure in coal caused by CO₂ are critical to CO₂ injection and CH₄ output in coal seams. To investigate the effects of CO₂ on the characteristics and connectivity of micron-scale pores and fractures in coal, four coal samples from the Qinshui basin were selected. These samples were exposed to CO₂ and water for 240 hours at 80 °C and 20 MPa using a CO₂ geochemical reactor. X-ray micro-CT (computed tomography), field emission scanning electron microscopy (FESEM), and energy dispersive spectroscopy (EDS) were used to identify the characteristics and connectivity of micron-scale pores and fractures in the coal samples before and after CO₂ treatment. Then, the influence of mineral dissolution on the micron-scale pores and fractures was discussed. After CO₂ treatment, the massive dissolution of carbonate minerals significantly increased the pore contents and volumes of the coal samples. For this reason, the grain size and volume of carbonate minerals determined the increase in pore number and volume after CO₂ treatment. The dissolution of calcite, dolomite, and other carbonate minerals in the coal matrix formed a large number of dissolution-created pores <10 ?m in diameter, which affected the pore number in the coal after CO₂ treatment but contributed little to the coal connectivity at the micron-scale. Carbonate minerals filling micro-fractures were heavily dissolved by CO₂, which increased the aperture and connectivity of the micro-fractures. The dissolution of carbonate minerals in micro-fractures was the major contributor to the increase in the volume of pores >50 ?m in diameter and the main reason for the increase in coal connectivity at the micron-scale.