Research Article
Effect of Temperature on the Thermal Conductivity of Rocks and Its Implication for In Situ Correction
Table 4
The depth and thermal conductivity of samples at Tarim Basin [
2].
| Lithology | Depth (m) | Estimated temperature (°C) | Porosity (%) | Fluid | Thermal conductivity (W/m·K) | Estimated thermal conductivity (W/m·K) |
| Dolomite | 6438 | 192 | 0.9 | Poor | 4.05 | 3.07 | Dolomite | 5815 | 175 | 1.8 | Poor | 3.64 | 2.94 | Dolomite | 4894 | 150 | 1.1 | Poor | 2.88 | 2.57 | Dolomite | 5579 | 169 | 4.5 | Poor | 2.32 | 2.16 | Limestone | 5158 | 158 | 2.5 | Rich | 2.48 | 2.30 | Limestone | 4911 | 151 | 4.3 | Rich | 2.23 | 2.14 | Limestone | 4515 | 140 | 0.9 | Poor | 2.14 | 2.08 | Limestone | 5221 | 159 | 4.5 | Poor | 2.71 | 2.44 | Limestone | 4257 | 133 | Void | Poor | 2.06 | 2.03 | Limestone | 5337 | 162 | 7.0 | Poor | 2.28 | 2.14 | Limestone | 5716 | 172 | 5.0 | Rich | 2.16 | 2.05 | Limestone | 6109 | 183 | 2.2 | Rich | 1.94 | 1.90 | Limestone | 5727 | 173 | 5.0 | Rich | 2.04 | 1.98 | Limestone | 6885 | 204 | 3.7 | Poor | 1.89 | 1.84 |
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