Fig. 8From: Validation of hydrogeochemical databases for problems in deep geothermal energySolubility of barite as a function of electrolyte in the solution at p = 1 bar and T = 100 \(^\circ \hbox {C}\) (except for data from Templeton (1960), which were measured at 95 \(^\circ \hbox {C}\)). Equilibrium calculations were executed at 100 \(^\circ \hbox {C}\). Values from Blount (1977) interpolated or extrapolated except for the values in 0.0, 0.2, and 4 molal NaCl solutionsBack to article page