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Fluid conductivity.
Black dot line represents fluid conductivity.
Conductivities are normalized by the fluid conductivity.
Its inverse gives the fluid conductivity.
The fluid conductivity is denoted by σ f.
Electrical conductivity is normalized by the fluid conductivity.
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Thus, target candidates for geothermal exploration are fractures and faults, which are (1) optimally oriented in the ambient stress state, (2) critically stressed for shear reactivation, and (3) show increased fluid conductivities due to alteration processes.
The correction to saline fluid conductivities from molecular dynamics data (Sakuma and Ichiki 2016) results in a 50%% increase of maximum salinities with respect to former estimates (Hyndman and Shearer 1989; Reynard, et al. 2011), without affecting substantially their general conclusions because salinities change over more than one order of magnitude.
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The FEA results demonstrate that (i) the overall effective thermal conductivity from direct simulations is comparable to the results estimated by experimental measurement, and are in the order of 10−1 W m−1 K−1 and (ii) thermal transport through fluid-saturated β-SiC foams depends on the solid-to-fluid conductivity ratio.
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