Research Article
Formation Mechanism of “Large-Area Sweating” Water Seepage from Deep Mine Sandstone Pores
Table 5
Hydrogeological features of three layers of sandstone aquifers.
| Aquifer features | Jurassic sandstone | Shihezi sandstone | Shanxi sandstone |
| Grain size | Medium, fine, and coarse sandstone and conglomerate | Medium and fine sandstone and a small amount of coarse sandstone | Medium and fine sandstone and a small amount of coarse sandstone | Thickness (m) | Single layer of 2.50-35.40; total thickness of 176.20-460.65 | Single layer of 2.70-30.25; total thickness of 34.50-270.80 | Single layer of 4.10-20.30; total thickness of 4.10-52.80 | Types of groundwater | Confined pore water and fracture water | Confined pore water and fracture water | Confined pore water and fracture water | Pore permeability | Medium-low | Low-ultralow | Low-ultralow | Fracture numbers | A small amount, developed locally near faults and folds | A small amount, developed locally near faults and folds | A small amount, developed locally near faults and folds | Main hydrochemical types | HCO3-·SO42--Na+ | SO42--Na+ | HCO3-·SO42--Na+ | Reservoir pressures (MPa) | 3.16-14.69 | 5.08-17.74 | 6.55-19.21 | Unit water inflow (L/s m) | 0.0471-0.1550 | 0.0039-0.0400 | 0.0020-0.0415 | Water abundance | Weak-moderate | Weak | Weak |
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