2015
DOI: 10.1016/j.apgeochem.2014.09.021
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Aqueous electrolyte solution modelling: Some limitations of the Pitzer equations

Abstract: Despite intense efforts, general thermodynamic modelling of aqueous electrolyte solutions still presents a difficult challenge, with no obvious method of choice. Even though the Pitzer equations seemingly provide a well-established theoretical framework applicable to many chemical systems over a wide range of temperatures and pressures, they are not as widely adopted as their early promise might have suggested. This is strikingly illustrated by the simultaneous appearance in the literature of numerous, differe… Show more

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Cited by 54 publications
(67 citation statements)
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“…These and other conspicuous failures of the Pitzer equations, 11 usually when the fit is not properly constrained by sufficient numbers of accurate data, infer an unreliability that casts doubt on the notion that the Pitzer equations possess any distinctive fundamental power. The term "semiempirical", which is widely used to describe the Pitzer equations, should perhaps mean more than just the sound foundation of Debye−Huckel theory represented in eq 1.…”
Section: Discussionmentioning
confidence: 96%
“…These and other conspicuous failures of the Pitzer equations, 11 usually when the fit is not properly constrained by sufficient numbers of accurate data, infer an unreliability that casts doubt on the notion that the Pitzer equations possess any distinctive fundamental power. The term "semiempirical", which is widely used to describe the Pitzer equations, should perhaps mean more than just the sound foundation of Debye−Huckel theory represented in eq 1.…”
Section: Discussionmentioning
confidence: 96%
“…[11]. Moreover, the Pitzer model requires use of both binary and ternary interaction parameters and the model offers no hints on temperature dependence of such interaction parameters [12,13]. The extended UNIQUAC model has been used for correlation and prediction of mineral solubility of Na + -K + -Cl À -SO 4 2À -H 2 O system at temperatures from 0 to 100 C [14].…”
Section: Introductionmentioning
confidence: 99%
“…It does not contain Fe as element, so no calculations can be performed for diagenetic Fe minerals such as siderite (FeCO 3 ), which is an important mineral in reservoirs and aquifers. In addition to its limited extent, the Pitzer database has some intrinsic shortcomings (Appelo, 2015;Rowland et al, 2015). A drawback of the regular database is the incorrect calculation procedure used to correct the concentration to activity for saline water.…”
Section: Geochemical Calculationsmentioning
confidence: 99%