Accurate characterization
of the compressibility of pores and fractures
in coal reservoirs is of great significance for predicting permeability
and for optimizing the production of coalbed methane (CBM). However,
for low-rank coal (R
o,max < 0.65%),
compressibility and the influences of different pore structures and
minerals on compressibility have not been studied thoroughly. To solve
this problem, four low-rank coal samples were collected from the south
of Junggar Basin. Low-field nuclear magnetic resonance is used to
study the compressibility of pore and fracture in low-rank coal and
its relationship with the heterogeneity. In addition, the effects
of fracture structure and minerals on compressibility were studied
by combining with micro-CT. The results show that the effects on the
compression space of the low-rank coal with the increase in effective
stress mainly come from the fracture and seepage pore volume, and
the compressibility becomes weaker. The low-rank coal reservoirs with
well-developed fractures and seepage pores show better compressibility.
The compressibility of the pores and fractures in low-rank coal is
noticeably affected by the mineral content, mineral shape, and mineral
arrangement. When the fracture development is similar, the coal reservoirs
with a high mineral content and with many fractures filled by minerals
show poor compressibility. There is a negative linear correlation
of the compressibility of pores and fractures with the fractal dimension
of the seepage space in low-rank coal. Moreover, the closing rate
of the pores and microfractures in low-rank coal with significant
heterogeneity in the seepage space is faster under confining pressure.
The research results are beneficial to the optimization of CBM production
measures in low-rank coal reservoirs.