In a facility for producing steam from a flow of silica-rich, naturally pressurized geothermal brine having volatile impurities, including ammonia, hydrogen sulfide and carbon dioxide, and having non-volatile impurities, including heavy metals, iron and calcium, the facility having high and low pressure flash crystallizers in which some of the steam is converted to steam and in which the flashed brine is contacted with seed crystals onto which silica deposits from the brine as the flashed brine becomes supersaturated in silica, having a reactor-clarifier stage in which the deposited silica is separated from the brine, and having a filtering stage for filtering clarified brine discharged from the reactor-clarifier stage, a method for combining with the flashed brine condensate from said steam, the condensate being basic and containing some of said volatile impurities which tend to react with said non-volatile impurities in the flashed brine to form fine, insoluble particles which are difficult to separate from the brine in the reactor-clarifier stage, and which, therefore, flow with the brine into the filtering stage, the method of combining the condensate with the brine comprising:
- (a) reducing the pH of the steam condensate to between about 7 and about 5.5 by contacting the condensate with an acidifying agent;
- (b) permitting the reduced pH steam condensate to outgas so as to reduce the concentration levels of the volatile impurities, especially of hydrogen sulfide and carbon dioxide;
- and,
- (c) combining the reduced pH, outgassed steam condensate with the flashed brine in the low pressure flash crystallizer.