Seepage pores are the main space
for methane transport in the coal
seam. To further investigate variation laws of seepage pores with
stress, this study established a new method based on the compressed
exhaust and pressure-transient tests to characterize the seepage pore
size distribution under different effective stress conditions. The
reconstituted coal briquette and nonabsorbent helium were adopted
as the experimental samples. The results showed that the deformation
of coal mass mainly originates from seepage pores. With the increase
of confining stress, the volume reduction of seepage pores presents
a logarithmic growth. The initial seepage porosity of the tectonic
coal specimen, i.e., the seepage porosity when effective stress is
zero, was estimated to be 5.28%, accounting for 36.24% of the total
porosity obtained by helium saturation. When effective stress is in
the range of 13–48 MPa, the size of seepage pores generally
ranges from 0.1 to 1.0 μm. The volume of seepage pores with
sizes ranging from 0.1 to 0.5 μm always accounts for more than
80% of the volume of total seepage pores, and this proportion is not
affected by effective stress. The inverse proportional coefficient
between the threshold pressure gradient of helium and seepage pore
diameter was finally determined to be 0.55 ± 0.19 mPa.