Electrolyte theory (e.g. Robinson and Stokes, 1965; Nordstrom and Munoz, 1985), addresses the behavior of solutions containing components such as sodium chloride which dissociate into ionic species. The term ‘electrolyte theory’ is generally used to address the properties of aqueous electrolyte solutions, usually at a fundamental level including the use of methods of statistical mechanics (e.g. Barker and Henderson, 1976; Mazo and Mou, 1979). The role of electrolyte theory in geochemistry is to help explain the physical chemistry and thermodynamics of natural waters, ranging from rainwater to concentrated brines (e.g. Nordstrom and Munoz, 1985).
The role of liquid water in aqueous solutions is primarily to act as the solvent. However, water is itself a weak electrolyte, dissociating according to the reactions:
The dissociation of acids (e.g. HCl, H2CO3), bases (e.g. NaOH, KOH), and salts (e.g. NaCl, CaCl2) into ionic species is favored by the high dielectric constant of water at...
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Bibliography
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Wolery, T.J. (1998). Electrolyte theory . In: Geochemistry. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4496-8_90
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