Determining the influence of gas pressure on the mechanics, permeability, and energy evolution of gas-bearing composite coal is helpful to better understand the formation process and prevention measures of gasdynamic disasters. In this paper, true triaxial mechanical-permeability tests are carried out on the gas-bearing composite coal rock under different gas pressures, focusing on the influence of gas pressure on the mechanics, permeability, and energy response characteristics of the composite coal rock, and a damage constitutive model based on energy dissipation is established. The results show that increasing the gas pressure decreases the load bearing capacity, strain, pre-peak relative permeability, and deformation capacity of the sample. The greater the gas pressure is, the greater the relative permeability decreases and the greater the post-peak relative permeability increases. The gas pressure has a great influence on the energy of the sample. The elastic strain energy ratio (Ue/U) increases with the increase in gas pressure, and the dissipative energy ratio (Ud/U) decreases with the increase in gas pressure. The coal-rock composite constitutive model based on energy dissipation is in good agreement with the experimental curves.

With the increasing frequency and intensity of coal and gas outburst disasters under deep mining conditions, studying the outburst mechanism of occurrence has great significance for outbursts prevention and control. The evolution law of coal and gas outbursts under different gas pressure is proposed. The outbursts law is analyzed utilizing the self-developed simulation experiment system of coal and gas outbursts, and the simulation experiment is carried out under the gas pressure of 0.45, 0.8, and 1.5 MPa. In the experiment, the gas pressure drops curves, the relative intensity change, the interval distribution of coal powder, and the evolution of outburst hole and the migration rate of coal powder are analyzed. The results indicate that (1) the gas pressure detected by the No. 4 gas pressure sensor starts to drop first; (2) the gas pressure is positively proportional to the relative outburst intensity. When the gas pressure increases from 0.45 to 0.80 MPa and then to 1.5 MPa, the farthest outburst distance of coal powder increases from 10 to 15 m and then to 21 m, and the corresponding relative outburst intensity increases from 22.94% to 35.74% and then to 45.73%, respectively. (3) The average proportion of coal particles size less than 0.28 mm and larger than 1 mm under each corresponding outburst interval is 40.75% and 22.53%, respectively. Experimental results show that the gas pressure plays an essential role in the secondary crushing and pulverization of coal samples during the outburst process. (4) The throwing velocity of the pulverized coal is increased with the gas pressure near the outburst hole. When the gas pressure is 0.8 MPa, the throwing velocity of pulverized coal reaches the maximum value of 32.40 m/s. (5) The dimensional characteristics and the location initiation of the outburst hole are obtained. The results showed that the outburst process of coal is mainly in two failure forms: pulverization and spallation. The research results provide a theoretical basis and test data support for the prevention and control of coal and gas outburst disasters.

The significance of coal mine gas control in the field of engineering cannot be underestimated

Transient gas transport in heterogeneous porous media subjected to thermal perturbation is a fundamental challenge in fluid dynamics. In this study, we investigated the thermal-driven evolution of pore topology and gas migration kinetics using coal as a representative multi-scale porous matrix. Isothermal adsorption and desorption experiments were conducted across various temperature gradients to quantify temperature-dependent gas–solid interfacial interactions, initial mass transfer rates, and volumetric release capacities. Both exponential and time-varying diffusion models were employed to characterize the non-isothermal gas diffusion kinetics. The results indicate that thermal perturbation significantly alters the geometric fractal characteristics of the solid matrix, leading to expanded pore volumes and increased topological complexity of the interfacial surfaces. Thermodynamically, elevated temperatures suppress the gas adsorption capacity while amplifying both the kinetic release rate and the intrinsic gas diffusion coefficient. Based on these fundamental mechanisms, an explicit mathematical expression for the time-varying dynamic diffusion coefficient during the initial transient stage of thermal perturbation is proposed. This work advances the fundamental understanding of non-isothermal gas transport mechanisms in complex porous networks, providing theoretical constraints for predicting fluid behavior under varying thermal boundary conditions.