Longwall mining of coal seams affects a large area of overburden by
deforming it and creating stress-relief fractures, as well as bedding plane
separations, as the mining face progresses. Stress-relief fractures and bedding
plane separations are recognized as major pathways for gas migration from
gas-bearing strata into sealed and active areas of the mines. In order for
strata gas not to enter and inundate the ventilation system of a mine, gob gas
ventholes (GGVs) can be used as a methane control measure. The aim of this paper
is to analyze production performances of GGVs drilled over a longwall panel.
These boreholes were drilled to control methane emissions from the Pratt group
of coals due to stress-relief fracturing and bedding plane separations into a
longwall mine operating in the Mary Lee/Blue Creek coal seam of the Upper
Pottsville Formation in the Black Warrior Basin, Alabama. During the course of
the study, Pratt coal's reservoir properties were integrated with
production data of the GGVs. These data were analyzed by using material balance
techniques to estimate radius of influence of GGVs, gas-in-place and coal
pressures, as well as their variations during mining.
The results show that the GGVs drilled to extract gas from the
stress-relief zone of the Pratt coal interval is highly effective in removing
gas from the Upper Pottsville Formation. The radii of influence of the GGVs were
in the order of 330–380 m, exceeding the widths of the panels, due to
bedding plane separations and stress relieved by fracturing. Material balance
analyses indicated that the initial pressure of the Pratt coals, which was
around 648 KPa when longwall mining started, decreased to approximately 150 KPa
as the result of strata fracturing and production of released gas. Approximately
70% of the initial gas-in-place within the area of influence of the GGVs
was captured during a period of one year.