The Ordos Basin is
a sedimentary basin located in Inner Mongolia,
China, where coal and uranium coexist. Water inrush disasters have
always been one of the main disasters that threaten the safety of
coal mine production, and thus, the study and division of groundwater
potential regions are of great significance for the prevention of
water inrush disasters and in situ leaching of sandstone-type uranium
ore. A new method combining truncated Gaussian simulation and sedimentary
facies control was established to predict the groundwater potential
area. Taking a typical aquifer, the Zhiluo Formation, as an example,
based on high-resolution sequence stratigraphy, geophysics, sedimentary
geology, and geostatistical theory, the plane distribution of sand
bodies was predicted. Furthermore, the relationship between rock porosity
and electricity porosity was established to calculate the regional
porosity. Combined with truncated Gaussian simulation and facies-controlled
modeling methods, a facies-controlled heterogeneous property model
was established to analyze the heterogeneous effective porosity of
the aquifer in the study area. Groundwater potential areas were quantitatively
evaluated by 3D modeling analysis. The results of the evaluated model
were verified by actual data and provide a geological guarantee for
the accurate mining of deep coal and uranium ore. A 3D distributed
model of chemical elements, which is meaningful for in situ leaching
uranium mining, is expected in future research.