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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