During the production process of coalbed methane, the
generation
and migration of coal fines can obstruct fractures in coal reservoirs
and reduce their permeability. In order to investigate the effects
of coal fines migration on the porosity and permeability of coal reservoirs,
we conducted core water flooding experiments, low-field nuclear magnetic
resonance (NMR), and low-temperature N2 adsorption experiments
to study the variations in porosity and permeability of cataclastic
coal during coal fines migration and the impact of coal fines migration
on porosity and permeability. The experimental results reveal that
the initial porosity ratio of cataclastic coal exhibits the characteristics
of micropore > macropore > transitional pore > mesopore,
with the
pore types being predominantly fissured. The porosity of pores larger
than 1000 nm and those larger than 10,000 nm exhibit consistent trends
before and after water flooding, indicating that the blockage or unblocking
of pores with radius larger than 10,000 nm by coal fines can also
cause blockage or unblocking of some interconnected macropore. The
early stage of flooding is the main period for coal fines migration
and production in cataclastic coal, during which the mass concentration
of coal fines production is higher and some macropores and fractures
become blocked, resulting in a larger decrease in porosity. The higher
the initial permeability of cataclastic coal samples with a larger
end-face fracture density, the more similar the variations in porosity
and permeability of pores larger than 10,000 nm during the flooding
experiment, indicating that coal fines mainly block interconnected
pores and fractures with radius larger than 10,000 nm through migration,
thereby reducing permeability. This study provides a theoretical basis
for the efficient production of coalbed methane.