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• W1980922260 abstract "A review of the sulfide scaling phenomena in low-temperature environments is presented. While high-temperature fluids tend to deposit metal sulfides because of their high concentrations of dissolved metals and variations of temperature, pressure and fluid chemistry, low temperature media are characterized by very low metal content but much higher dissolved sulfide. In the case of the geothermal wells of the Paris Basin, detailed studies demonstrate that the relatively large concentrations of chloride and dissolved sulfide are responsible for corrosion and consequent formation of iron sulfide scale composed of mackinawite, pyrite and pyrrhotite. The effects of the exploitation scheme are far less important than the corrosion of the casings. The low-enthalpy fluids that do not originate from sedimentary aquifers (such as in Iceland and Bulgaria), have a limited corrosion potential, and the thin sulfide film that appears may prevent the progress of corrosion." @default.
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• W1980922260 date "1989-01-01" @default.
• W1980922260 modified "2023-10-14" @default.
• W1980922260 title "Sulfide scaling in low enthalpy geothermal environments: A survey" @default.
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• W1980922260 doi "https://doi.org/10.1016/0375-6505(89)90012-6" @default.
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