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Table 3 Ranges of tested values during the back analysis called “prior distributions”
From: THM modeling of hydrothermal circulation at Rittershoffen geothermal site, France
Property (unit) | Upper sediments | Lower sediments | Upper granite | Lower granite |
|---|---|---|---|---|
Permeability \(K_{\text{int}}\) (m\(^2\)) | 10\(^{-21}\)–10\(^{-15}\) | 10\(^{-21}\)–10\(^{-15}\) | 10\(^{-21}\)–10\(^{-11}\) | 10\(^{-21}\)–10\(^{-11}\) |
Thermal conductivity \(\lambda _d\) (W m\(^{-1}\) K\(^{-1}\)) | 0.4–6.5 | 0.4–6.5 | 0.4–6.5 | 0.4–6.5 |
Young’s modulus E (GPa) | 5.0–95.0 | 5.0–95.0 | 5.0–95.0 | 5.0–95.0 |
Poisson’s ratio \(\nu\) (–) | 0.05–0.49 | 0.05–0.49 | 0.05–0.49 | 0.05–0.49 |