Tectonic action strongly impacts the coal's microcrystalline and pore structural features. X-ray diffraction (XRD) was employed to analyze the impact of tectonic action on the microcrystalline structure of coal. The pore structure of anthracite was investigated through electron microscope image, mercury intrusion porosimetry and low pressure N2/CO2 adsorption, with a focus on exploring the relationship between the microcrystalline structure of coal and its micropore structure. The results show that under tectonic action, interlayer spacing of the aromatic layer d002 decreases from 0.345 to 0.342 nm, the stacking height Lc decreases from 2.73 to 2.23 nm, the average number of the effective aromatic layer Nave slightly decreases from 6.61 to 6.51, and the crystallite diameter La increases by 0.13 nm, which indicates that tectonic action changes the microcrystalline structure of anthracite. The microcrystalline structure changes from "short and thick" to "long and thin", thus schematic diagram of the anthracite basic structural unit (BSU) under tectonic action was established. The fa of tectonic coal increased by 16.92% compared with that of original coal, and the g increased from 0.85 (original) to 0.89 (tectonic), indicating that the process of aromatization and graphitization of coal was accelerated by tectonic action. Tectonic action plays an important role in promoting pore development, which makes the pore surface of anthracite more rough, the lattice fringe more dense and clear, and increases the pore volume and specific surface area of anthracite by 1.21 and 1.08 times, respectively. Tectonic action can change the BSU of coal, thus producing more nanoscale space. This study holds important implications for comprehending how tectonic action affect the microcrystalline structure of coal as well as its relationship with nanopore structures in tectonic coal.
Read full abstract