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• W4361027797 endingPage "102710" @default.
• W4361027797 startingPage "102710" @default.
• W4361027797 abstract "The global demand for sustainable and clean renewable energy sources is rapidly increasing to meet growing energy demands while curtailing the CO2 emissions from fossil fuels. Harnessing the natural heat or geothermal energy of the Earth's interior can simultaneously address both issues by offering a clean and renewable energy source. Enhanced geothermal systems require the movement and cycling of fluid through a porous rock media. This process requires understanding the chemistry occurring at the fluid-rock and fluid-metal interfaces both in the deep subsurface and surface, where fluid is circulated for energy transfer or storage. In this review paper, we evaluate the current state of research on how two key variables, pH and Eh, control the fluid-rock reactions controlling mineral scaling and the steel corrosion reactions associated with geothermal systems. These variables are frequently used in geochemical modeling to predict chemical reactions in geothermal systems. Prediction of the fluid-rock behavior can be utilized to formulate new strategies for extending the lifespan and efficiency of heat extraction and utilization and maximizing the safety of geothermal systems." @default.
• W4361027797 created "2023-03-30" @default.
• W4361027797 creator A5025546371 @default.
• W4361027797 creator A5057268341 @default.
• W4361027797 creator A5067390670 @default.
• W4361027797 date "2023-06-01" @default.
• W4361027797 modified "2023-10-11" @default.
• W4361027797 title "Role of pH and Eh in geothermal systems: Thermodynamic examples and impacts on scaling and corrosion" @default.
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