Fracturing fluid is a key factor affecting the hydraulic
fracture
morphology and coal microstructure, which plays a key role in the
hydraulic fracturing effect. To compare the effect of clean water,
clean fracturing fluid, and acid fracturing fluid on the pore structure
of coal, this paper used high-pressure mercury injection (MIP), low-temperature
N2 adsorption (LT-N2A), and scanning electron
microscopy (SEM) to determine the pore structure of Guizhou bituminous
coal before and after the action of fracturing fluid. The results
show that clean water can cause mineral expansion and reduce pore
volume by about 6% and clean fracturing fluid and acid fracturing
fluid can increase pore volume by 3 and 12%, respectively, due to
different degrees of acidity. The MIP data show that the pore structure
of coal samples is more complex after the action of different fracturing
fluids, and acidic fracturing fluids can increase the fractal dimension
of the pore by about 7%. The LT-N2A data showed that the
fractal dimension of micropores and transition pores decreased after
the action of different fracturing fluids. In general, acid fracturing
fluid has the best effect on the coal microstructure, followed by
clean fracturing fluid, and the least effect on clean water.