Accurate and reliable
evaluations of potential groundwater areas
are of significance in the hydrogeological assessments of coalfields
because water inrush disasters may be caused by unclear groundwater
potential. A three-dimensional geological model of porosity based
on deterministic modeling and a facies-controlled method are used
to determine the groundwater potential of the coal measure aquifer.
The modeling processes are as follows: based on the interlayer and
discontinuity (faults) data extracted from boreholes and geological
maps, an integrated sequence framework model is developed. Using the
results of sedimentary microfacies identification and the method of
deterministic modeling, a sedimentary microfacies model is successfully
established. Finally, based on facies-controlled and sequential Gaussian
methods, an effective porosity model is established that can predict
the groundwater potential. The predicted results show that sandstones
sedimented in channel, point bar, and batture environments possess
high effective porosity and strong groundwater potential; however,
the sandstones sedimented in interdistributary bays, flood plains,
and sand sheets possess low effective porosity. Model validation was
performed based on the hydrological pumping test data collected from
observation boreholes, drainage water inflow data from dewatered boreholes
in the tunnel around workface, and the mine water inflow in tunnels
and the workfaces. The validation analysis results show that the effective
porosity and sedimentary facies were correlated with the actual flux.
The predicted results are consistent with the actual flux data, validating
the predicted model.