Shale–persulfate
interactions commonly occur in shale hydraulic
fracturing, but the interaction mechanism and its implications for
shale matrix alteration remain poorly understood. In this study, interactions
between shale collected from Yichang, Hubei Province, China, and persulfate
were investigated with experiments and geochemical modeling. The results
revealed that although significant gypsum precipitation offsets the
mass loss caused by pyrite, kerogen, and carbonate dissolution, the
enlargement of micropores in shale still occurred when treated with
persulfate. Both Fourier transform infrared spectroscopy and water
chemical analyses confirmed that pyrite was preferentially oxidized
by persulfate and that aliphatic C–O or −COOH was generated
in kerogen after the treatment with persulfate. The oxidation rate
of pyrite was 1.82 × 10–4 mol·m–2·s–1 according to the numerical simulation
results, which was 1.5-fold higher than kerogen. Calcite, dolomite,
and chlorite were all favorable for kerogen oxidation by inhibiting
decomposition and prolonging the life cycle of persulfate. Dolomite
showed priority in promoting kerogen oxidation over calcite and chlorite.
According to the geochemical simulation, the key components, including
calcite, pyrite, kerogen, dolomite, chlorite, and gypsum, contributed
to −42.9, −16.6, −4.9, −3.7, −5.1,
and 61.1% of the total solid mass change, respectively.