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出典:『Wikipedia』 (2011/03/23 08:39 UTC 版)

英語による解説

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Pitzer equations are important for the understanding of the behaviour of ions dissolved in natural waters such as rivers, lakes and sea-water. The parameters of the Pitzer equations are linear combinations of parameters, of a virial expansion of the excess Gibbs free energy, which characterise interactions amongst ions and solvent. The derivation is thermodynamically rigorous at a given level of expansion. The parameters may be determined by measuring osmotic coefficients. They can be used to calculate single-ion activity coefficients in solutions which for which Debye–Hückel theory is inadequate. They are more rigorous than the equations of specific ion interaction theory (SIT theory), but Pitzer parameters are more difficult to determine experimentally than SIT parameters.