1980
DOI: 10.1139/v80-196
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Activity corrections for ionic equilibria in aqueous solutions

Abstract: for ionic equilibria in aqueous solutions at 2S°C and ionic strengths up to 0.5 have been investigated. An empirical formula for activity corrections was generated by statistically fitting stability constant data for approximately 540 complexes. for which both thermodynamic and concentration stability constants were known, to a modified Debye-Huckel relationship. The general formula isx > 0, where A log K is the difference in the logarithms of the stability constants at infinite dilution and finite I ( I 5 0.5… Show more

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Cited by 44 publications
(42 citation statements)
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References 5 publications
(10 reference statements)
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“…GEOCHEM calculations for an A1 oxalate solution (Al:ox molar ratio 1:2, pH 3.9), in which NMR integration estimated 11.3% of the A1 to be present as the Alox3 species, gave low estimates for this species suggesting that the constants in the databases are incorrect. Editing the database of GEOCHEM-PC v. 2.0 with other literature constants (Perrin, 1979), corrected to zero ionic strength (Sun et al, 1980), for all three A1 oxalate complexes gave results that more closely matched the NMR integral values (Table 1).…”
Section: Discussionmentioning
confidence: 58%
“…GEOCHEM calculations for an A1 oxalate solution (Al:ox molar ratio 1:2, pH 3.9), in which NMR integration estimated 11.3% of the A1 to be present as the Alox3 species, gave low estimates for this species suggesting that the constants in the databases are incorrect. Editing the database of GEOCHEM-PC v. 2.0 with other literature constants (Perrin, 1979), corrected to zero ionic strength (Sun et al, 1980), for all three A1 oxalate complexes gave results that more closely matched the NMR integral values (Table 1).…”
Section: Discussionmentioning
confidence: 58%
“…Combination of Equilibria (1) -(4) with the thermodynamic equilibrium constant Kl corrected for the changes in ionic strength according to Eq. (9) from [12] furnishes very concordant values of the various parameters for all curves with the exception of the isohydric at C H = 0.5 M. The parameters derived when fitting all curves together are given in Table 2 and the calculated curves are shown as solid lines in Figs. 1 and 2 and as dashed lines in Fig.…”
Section: Data Analysis: Role Of Fe 3+ Ion Pairing With CImentioning
confidence: 67%
“…It is important to notice that the Raman-derived binding constants for the contact ion pairs (or equivalently binding free energies) are obtained at finite ionic strength (between ~0.3 and ~1.5 M), while calculated binding free energies correspond to a standard binding free energy in the infinite dilution limit. Hence, to compare measured and calculated binding free energies, we first extrapolated the experimentally-derived binding free energies to zero ionic strength, using a refined Davies 45,46 -like equation fitted on a large set of ion-ion binding constants measured at different ionic strengths. 46 We thus report in Table 1 the extrapolated experimental binding free energy, which can be directly compared with the computed contact binding free energy, that encompasses both monodentate and bidentate binding geometries.…”
Section: Resultsmentioning
confidence: 99%
“…Hence, to compare measured and calculated binding free energies, we first extrapolated the experimentally-derived binding free energies to zero ionic strength, using a refined Davies 45,46 -like equation fitted on a large set of ion-ion binding constants measured at different ionic strengths. 46 We thus report in Table 1 the extrapolated experimental binding free energy, which can be directly compared with the computed contact binding free energy, that encompasses both monodentate and bidentate binding geometries. Note that these extrapolated binding free energies are still quite small, around −3.2 kJ mol −1 for Ca 2+ , −3.4 kJ mol −1 for Mg 2+ , and only −6.9 kJ mol −1 for Zn 2+ .…”
Section: Resultsmentioning
confidence: 99%