Low-temperature oxidation leads to the accumulation of
heat in
coal, and it is an important trigger for coal spontaneous combustion
(CSC). The oxidation effects induce irreversible damage in the pore
and fracture structures of coal, which provide a way for the infiltration
of oxygen. In this work, the evolution of pores and cracks of coal
in the progress of low-temperature oxidation is researched based on
nitrogen adsorption, scanning electron microscopy (SEM), and ultrasonic
testing. The results show that the oxidation effect increases microporous
structures and promotes the development of mesopores and macropores
in coal. Besides, as the temperature increases, the oxidation effect
becomes more significant, while the pore morphology has not changed
significantly yet. Meanwhile, the oxidation effect causes coal particles
to block or collapse in the macropores, and the plugging degree increases
with increasing temperature.