Coal structure, including
primary coal, cataclastic coal, granulated
coal, and mylonitized coal, is one of the key factors controlling
coal and gas outburst, and it also determines the efficiency of coalbed
methane (CBM) extraction. Therefore, it is significant to identify
the characteristics of coal structures and to predict them in advance.
In this work, the spatial distribution, mechanical properties, and
microscopic morphology of the four coal structures from the No. 3
coal seam of the Xinyuan Mine in the northern part of the Qinshui
Basin were investigated through the in situ observation in the roadway,
the hardness coefficient (
f
) test, and the scanning
electron microscope analysis. Moreover, the drilling cuttings from
the gas pressure releasing holes were sampled and sieved, and then,
the correspondence between different coal structures and the particle
size of the cuttings was analyzed quantitatively based on the Rosin–Rammler
model. The result shows that the spatial distribution of the coal
structure has strong heterogeneity in the vertical and lateral directions.
The
f
value decreases successively with the increase
in coal structure deformation, which indicate that
f
can directly characterize the coal structure. Furthermore, the relations
between
f
and drilling cutting average particle size
(
d
0
), crushability indicator (
n
), crushing degree index (λ), and the median diameter
(
d
50
) were established. Specifically,
the coal deformation degree is positively correlated with the mass
fraction of large particles in the cuttings under the same drilling
parameters. Overall, as
f
increases,
d
0
and
d
50
decrease, and
n
and λ increase. However, parameters
d
0
,
d
50
, and λ of granulated
coal are inconsistent with other coal structures, and mylonitized
coal is inconsistent with other coal structures in
n
, as a result of the coal structure broken characteristics itself
and the difference in the stress state between the coal and the drill
bit during the rock breaking process. Ultimately, the coal structures
determined by the surface CBM well logging curve and the cuttings
particle size method were compared, and they have a high degree of
coincidence in the distinction between primary coal and tectonic coal.