Coal pore size distributions controlled by the coalification process: An experimental study of coals from the Junggar, Ordos and Qinshui basins in China

•Pore size distributions of different rank coals were systematically studied.•Key variation points of coal pores evolution were recognized.•Explanation of the factors controlling pores characteristic was presented.•The physical parameters of coals from three typical CBM basins in China were studied. Various sizes of pores in coal, which are generally formed by organic matter during the coalification process, have a direct influence on coalbed methane extraction. However, few studies have investigated the pore size distributions across the thermal evolution of coal from peat to anthracite. In this project, three series of coal samples collected from three key CBM development basins with graded vitrinite reflectance values (Ro), the eastern Junggar basin (Ro of approximately 0.5%), eastern Ordos basin (Ro of approximately 2.2%) and southern Qinshui basin (Ro of approximately 3.0%), were systematically characterized by optical observations, low-temperature nitrogen adsorption/desorption, and nuclear magnetic resonance (NMR) methods. The average pore radius calculated by the Brunauer-Emmett-Teller (BET) method shows that the low-rank (L) series (averaging 14.17nm) has values higher than either the middle-rank (M, 12.70nm) or high-rank (H, 12.66nm) samples. Bright and semi-bright coals (determined by the overall relative lustre and percentage of bright components) are generally distributed with relatively higher pore radii (averaging 16.86nm for all 3 series) than the semi-dull and dull coals (9.50nm). The range of pore sizes decreases as the coal rank increases, and the NMR transverse relaxation (T2) spectrum decreases from bi-modal and tri-modal (M and L series) to unimodal curves (H series). However, the pore surfaces and complexity inside the coal increase with the coal rank, with the fractal results showing a three-stage fitting slope of the H series compared with the M (two-stage) and L (one-stage) coals. The observations are generally caused by the L coals, which mainly include plant tissue pores, while the M series coals are characterized by circle-shaped tissue pores and gas pores. The H series of flattened tissue pores and more diverse gas pores are identified in the higher-rank coals. Combined with the thermogenic gas generation process of coal, three key transition points were recognized: (1) Ro of approximately 0.5%, transition of dehydration to bituminization with coals being much more compacted, shown as the >100nm range pores decreasing sharply;