Gas transport within the coal matrix is key to realizing mass exchange between the fracture and matrix systems. However, considerable controversy remains regarding gas transport within the coal matrix system. In this study, the applicability of several typical models was evaluated based on the proposed criteria, mainly through gas emission under pressure experiments, and it is found that the Darcy seepage model describes gas transport behavior within the coal matrix more scientifically. Subsequently, the validity of the seepage model was re-evaluated through pore structure analysis, and the gas transport patterns and underlying mechanisms of the dual-porosity and dualpermeability models were discussed. The results suggest that gas transport within the matrix is dominated by the Fick diffusion flow only when methane molecules within the coal matrix are located in the micropore filling section. When the pore size is located in the outer pore section, gas within the matrix will be transported outward in a free state driven by pressure. In addition, the proposed gas transport model and field data were used to validate the analysis. It is concluded that in view of the low efficiency of gas transport in the micropore filling section, the dual-porosity and doublepermeability models can be used to simplify gas transport in coal seams.