1977
DOI: 10.1039/dc9776400274
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Precise conductimetric studies on aqueous solutions of 2:2 electrolytes. Interpretation of new data in terms of the current theories of Pitt and Fuoss

Abstract: New, precise data are reported for the conductivity of magnesium sulphate in water at 25 and 5 0 T . The data are analysed using the Pitts, Fuoss (1975) and Carman conductance equations and the Debye-Huckel and Glueckauf activity coefficient equations. The Fuoss (1975) equation combined with the Debye-Hiickel equation is found to give the best fit of the data, but only over a limited concentration range.

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Cited by 24 publications
(5 citation statements)
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“…The results for K A are plotted in Figures and , along with values obtained by conductance methods from other workers. , Values for MgSO 4 determined by Marshall from solubility measurements are included in Figure for comparison. The association constants for both systems show a rapid increase with temperature.…”
Section: Resultsmentioning
confidence: 99%
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“…The results for K A are plotted in Figures and , along with values obtained by conductance methods from other workers. , Values for MgSO 4 determined by Marshall from solubility measurements are included in Figure for comparison. The association constants for both systems show a rapid increase with temperature.…”
Section: Resultsmentioning
confidence: 99%
“…Temperature dependence of equilibrium constants log( K A ) for the MgSO 4 (aq) system: ●, this work; △, Marshall solubility; ◻, Katayama conductance; ○, Nair and Nancolas EMF; ⧫, Tomsic et al, conductance; ×, Pethybridge and Taba; , eq .…”
Section: Resultsmentioning
confidence: 99%
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“…Limiting molar conductivities for HCI as a function of temperature are tabulated in Table II. These were calculated first with the conductance function proposed by Fuoss in 1975 (16) using a computer program developed by Pethybridge (17) which searched for that value of the distance parameter, R, that would give the best fit of the data to the function. However, the range of concentrations available did not include high enough concentrations to generate a minimum in the residuals of significant depth as the Gurney sphere diameter, R, was varied.…”
Section: Resultsmentioning
confidence: 99%
“…74,75 Επίσης, σε υδατικά διαλύματα η σύζευξη ιόντων είναι σπάνια για μονοσθενείς συμμετρικούς ηλεκτρολύτες αλλά είναι πολύ σημαντική για δισθενείς ηλεκτρολύτες. 76 Χαρακτηριστική είναι η παρατήρηση των Pethybridge και Taba, 77 οι οποίοι αναφέρουν ότι διαλύματα συμμετρικών 2:2 ηλεκτρολυτών σε νερό είναι ισοδύναμα με διαλύματα 1:1 ηλεκτρολυτών σε ένα διαλύτη με διηλεκτρική σταθερά ~20. 73,78 Όταν η διηλεκτρική σταθερά του διαλύτη είναι πολύ μικρή (σε μη υδατικούς διαλύτες), οι ηλεκτροστατικές δυνάμεις είναι πολύ ισχυρές, με αποτέλεσμα τα ιοντικά ζεύγη (Μ + Α -), να έλκουν ιόντα για να σχηματίσουν σύμπλεγμα τριών ιόντων [ΜΑΜ] + ή [ΑΜΑ] -:…”
Section: λαμβάνοντας υπ'όψιν αυτές τις παραδοχές και γνωρίζοντας ότι 1000 /unclassified