Research Article
Effects of Thermal Water Upwelling on Microclimate Change in the High Geo-Temperature Roadway
Table 2
Impermeability and thermal conductivity of strata in Sanhejian Coal Mine [
34,
35].
| Era | Period | Code | Lithology | Thickness (m) | Aquosity | Geothermal gradient () | Thermal conductivity | Terrestrial heat flow () |
| Cenozoic | Quaternary | Q | Clay, sand | 220 | Weak | 3.5 | | | Mesozoic | Cretaceous | K | Sandstone, glutenite, mudstone | 391 | Weak | 2.8 | 2.74 | 76.6 | Jurassic | J | Sandstone, mudstone |
| Paleozoic | Permian | P | Mudstone, sandstone, coal, limestone | 536 | Weak | 3.3 | 2.28 | 75.1 | Carboniferous | C | 3.3 | 2.22 | 76.1 | Ordovician | O | Limestone, dolomite | 500–742 | Water abundance and strong permeability | | 2.94 | |
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