Fig. 1From: Quantification of the effect of gas–water–equilibria on carbonate precipitation(left): Schematic figure of geothermal facility highlighting boundary conditions for pressure and temperature which drive the disruption of the lime-carbonic acid-equilibrium, and (right): experimental design to address processes occurring above the submersible pump (highlighted in red) and the disruption of the lime-carbonic acid equilibrium by the presence of a free gas phaseBack to article page