摘要
Based on the coal proximate,coal maceral composition and low-temperature N2 adsorption analyses, microfracture analysis by fluorescence microscope, helium porosity and air permeability analyses, this paper investigated the geological control of porosity and permeability of coals in Hedong, Weibei, Yangquan, Jincheng, Datong and Huainan-Huaibei coalfields. The results showed that coal porosity ranged from 2% to 10%, and strongly related to the coalification degree. The porosity reached a minimum value when Ro, r was about 1.2%. The filling and mineralization of pores by minerals were proven to decrease the coal porosity. Coal permeability is commonly less than 5×10-3 μm2, and shows an exponential increment relationship with porosity. The anthracite porosity is commonly less than 6%, which dominated by the micro-and meso-pores porosity.