In this study, the dominant path of hydrocarbon generation
in supercritical
water of granular medium- and low-maturity organic-rich shale is determined
as well as the mechanism of supercritical water in the process of
hydrocarbon generation of granular medium- and low-maturity organic-rich
shale. The kinetics of hydrocarbon generation in supercritical water
from granular medium- and low-maturity organic-rich shale was studied.
A dynamic model of the hydrocarbon generation reaction of granular
medium- to low-maturity organic-rich shale in supercritical water
was constructed. The Runge–Kutta fourth-order algorithm and
basin hopping algorithm were used to solve the fitting parameters.
The model consisted of 11 parallel first-order reactions, which could
accurately predict the mass fraction of the hydrocarbon generation
products of granular medium- and low-maturity organic-rich shale in
supercritical water and reveal the mechanism of the hydrocarbon generation
reaction of medium- and low-maturity organic-rich shale in supercritical
water. It was found that the hydrocarbon generation pathways of granular
medium- and low-maturity organic-rich shale in supercritical water
mainly consisted of direct generation of asphaltenes and saturated
hydrocarbons from kerogen, pyrolysis of asphaltenes to saturated hydrocarbons,
aromatic hydrocarbons, and resins, polymerization of resins to asphaltenes,
and gas generation from saturated hydrocarbons, resins, and asphaltenes.
The role of supercritical water facilitated the direct generation
of saturated hydrocarbons from kerogen.