Research Article

Effect of Strain-Dependent Hydraulic Conductivity of Coal Rock on Groundwater Inrush in Mining

Table 3

Parameters and lithology of the numerical model of water inrush in the working face.

LithologyThickness (m)Density (kg/m3)Elastic model (GPa)Poisson’s ratioCohesion (MPa)Tensile strength (MPa)Internal friction angle (°)Dilatancy angle (°)Hydraulic conductivity (×10-6 cm/s)Porosity

Roof10026005.000.253.02.6322410.80.2
Siltstone625502.300.272.62.532233.00.15
Fine sandstone1226005.000.253.02.8322410.80.2
Mudstone3.525001.450.351.31.030221.00.1
Fine sandstone1626005.000.253.02.8322410.80.2
Siltstone425502.300.272.62.532233.00.15
No. 8 coal3.520001.400.31.21.028221.00.1
Siltstone825502.300.272.62.532233.00.15
Mudstone425001.450.351.31.030221.00.1
Fine sandstone426005.000.253.02.8322410.80.2
Siltstone1025502.300.272.62.532233.00.15
Floor3426005.000.254.03.2322410.80.2