“…Pyrolysis approximates the natural processing of the organic material in the shale, i.e., kerogen, using higher temperatures to compensate for the geological time frame. 71 Upon heating, kerogen decomposes by consecutive reactions into a benzene-soluble material (pyrolytic bitumen), which, in turn, decomposes to form the final products of oil, gas, and carbonaceous residue on the spent shale: 71 The series of reactions taking place during the process is illustrated in eq 10 where Kr is the kerogen, Pb is the pyrolytic bitumen, Og is oil and gas and Oc is the organic carbon residue. 71 The mathematical model in eq 11 describes the evolution of the concentrations, C Kr , C Pb , C Og , and C Cr , where k i is the specific reaction rate, k i0 is its initial value, E i is the activation energy, R is the gas constant, and T is the temperature that can be manipulated within the range of [698.15 ≤ T ≤ 748.15].…”