Gas diffusion in a coal seam plays an essential role
in the efficient
and effective exploitation of underground coalbed methane (CBM). Based
on the concept of free gas density gradient-driven flow, in this work,
we formulated and validated a theoretical model to quantify gas desorption
and diffusion kinetics in a coal seam at different temperatures. Once
the governing equations are formulated and non-dimensionalized, they
are numerically solved with the finite difference method and then
validated with the experimental measurements on gas desorption at
different temperatures. The mechanism of temperature affecting gas
diffusion kinetics was elaborately explored. Also, the advantages
of the proposed free gas density gradient model (FGDGM) compared to
the traditional unipore diffusion model (UDM) were well evaluated
and discussed. It is found that the FGDGM simulations are basically
consistent with the experimental data, but the UDM prediction deviates
significantly from the experimental measurements at different temperatures.
By introducing a new dimensionless temperature variable and performing
sensitivity analysis, the dimensionless gas desorption is found to
increase with temperature, while the incremental gas desorption varies
across the entire temperature range. With the temperature increasing
from 293 to 313 K, both the gas desorption increment and gas yield
enhancement are found to be the largest. In addition, there exists
a linear relationship between diffusivity and temperature because
a high temperature increases the gas molecules’ activity and
accelerates the pore expansion. It is clearly found that temperature
has a considerable contribution to the gas diffusion kinetics in a
coal seam, and appropriately boosting the coal temperature to enhance
CBM recovery is feasible and valuable.