During the development of deep coalbed methane resources, the impact caused by mining disturbance has a significant effect on the evolution of coal pore-fracture and permeability characteristics. Revealing the damage mechanism and gas seepage law of coal in the mining process can provide important basis for the efficient exploitation of coalbed methane. Dynamic impact tests were conducted using the Split Hopkinson Pressure Bar (SHPB) testing system, the T2 relaxation spectrum and permeability of the impacted coal were measured, respectively. The evolution of pore damage and permeability in coal samples was analyzed from the perspective of energy dissipation. The results showed that as impact pressure increases, adsorption and seepage pores successively dominate the evolutionary process, and the pore fractal dimension of coal samples first increases and then decreases. Magnetic Resonance Imaging (MRI) images reveal obvious linear concentrated damage zones, and these zones lead to the overall evolution of pore structure from point-like dispersion to complex linear interweaving. The permeability of coal samples increases as the impact pressure increases. Under the same impact pressure conditions, the permeability decreases exponentially with an increase in gas pressure. The dissipation energy density and damage variable of coal samples both increase exponentially with the increase of impact pressure. Impact disturbances significantly affect the expansion of pores and fractures in coal. As the damage variable increases, both the porosity and permeability increment of the coal sample exhibit a linear increasing trend. As the extraction time of the test working face increases, the energy of microseismic events and the absolute gas emission show an increasing trend. This indicates that the effect of impact wave causes the gas seepage channel of coal expand, and the permeability enhancement effect is significant.
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