In the Netherlands, well monitoring and fluid sampling campaigns were carried out to assist in understanding the injectivity decline in several geothermal wells used for heating greenhouses. As part of these campaigns, ref. gathered the chemical analyses at several sites from different geological formations in the Netherlands (e.g., Carboniferous, Rijswijk, Slochteren). In the mentioned report, the bubble point pressures at six sites were reported. Yet, among these six sites, only for three of them, the GLR ratio was included as well. Among the three sites that include both the bubble point pressure and the GLR, the gas composition is available only for one of them. Thus, only one experimental measurement (corresponding to site 3 in the mentioned report, Rijswijk formation) can be used for comparison to the bubble point pressure predicted by PHREEQC and Reaktoro. The composition of the fluids, i.e., gas and liquid, sampled at this site and the GLR are reported in Table . Note that the original reference does not clearly state whether the GLR is reported at standard conditions but for the calculations, it has been assumed so.