“…The important conclusions are as follows: (1) Montmorillonite transforms into kaolinite and illite in OP, and into illite to form an illite/montmorillonite mixed layer in AR. (2) The specific surface area and pore volume of semi-cokes are extremely low at low temperatures in AR, whereas numerous mesopores and macropores can be formed in OP, leading to significant increases in the specific surface area and pore volume even at low temperatures. (3) Variations in chemical composition and pore evolution of semi-cokes obtained via AR and OP affected their thermophysical properties.…”