The
study of the microstructure evolution law of coal in a natural
reservoir environment for the extraction of coalbed methane mining
(ECBM), especially deep ECBM, is of major significance. We treated
coal samples from Qinshui Basin under combined temperature–gas–fracturing
fluid conditions and analyzed the evolution of the microstructure
and its fractal characteristics to study the microstructural evolution
of coal under natural hydraulic fracturing conditions. In the temperature
range of 303.15 to 343.15 K and the gas-pressure range of 0.5–4.5
MPa, our data demonstrate that the pore structure is more susceptible
to the temperature influence, compared with microfracture. The treatment
of viscoelastic surfactant fracturing fluid (VES-FF) can effectively
increase the permeation pore and fracture ratio by more than 300%
and reduce the adsorption pore by more than 200% through dissolution,
gas wedge, and other effects, which is favorable to ECBM. At the same
temperature, as the gas pressure increases, the pore decreases, whereas
the fracture ratio increases. The pore fractal dimension ranges from
2.90 to 2.99, which is significantly higher than that of microfractures.
The temperature has a minor effect on the fracture fractal dimension,
but it causes a decrease in the pore fractal dimension. The treatment
of VES-FF induces an increase in the fracture fractal dimension, implying
an increase in the fractal complexity. In contrast, the pore fractal
characteristics show a contrary trend. At a gas pressure of 4.5 MPa,
the negative effect of VES-FF on the pore structure reaches its maximum,
whereas the effect on the fracture drops to its minimum. The results
document that high temperature and high gas pressure can severely
limit the penetration enhancement effect of VES-FF.