1969
DOI: 10.1021/j100725a049
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Solubility and complex formation equilibria of silver chloride in dimethyl sulfoxide-water mixtures

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Cited by 45 publications
(6 citation statements)
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“…(12) shows that no difference can arise between the two scales in the concentration range here employed. The validity of the Lkbye-Hiickel corrections, and especially the arbitrary choice of the ion size parameter seems to be justified by the fact that our experimental pKs value at 2 5 T , when corrected from I = 0.01 to I = 0.1 amounts to 10.27+0.02 which agrees with the value of 10.279f0.003 obtained by Synnott and Butler [2] in 0.1 M LiClO,.…”
Section: Resultssupporting
confidence: 79%
See 1 more Smart Citation
“…(12) shows that no difference can arise between the two scales in the concentration range here employed. The validity of the Lkbye-Hiickel corrections, and especially the arbitrary choice of the ion size parameter seems to be justified by the fact that our experimental pKs value at 2 5 T , when corrected from I = 0.01 to I = 0.1 amounts to 10.27+0.02 which agrees with the value of 10.279f0.003 obtained by Synnott and Butler [2] in 0.1 M LiClO,.…”
Section: Resultssupporting
confidence: 79%
“…The principal equilibria involved during titration of a AgN03-DMSO solution with LiCl are: Solid silver chloride precipitates until the first equivalence point ( u~,~) is reached. Then the solid dissolves, forming the complex AgC12-and the second equivalence point is reached (ue,*), after which equilibrium (2) persists.…”
Section: Theorymentioning
confidence: 99%
“…(1) -8; (2) -6; (3) -4; (4) -2; (5) 0; (6) +2; z = -1; ci/e0 = % log ßlog ß°-0.022 = 0.2981<7m ~0.0197qM2 (24) Therefore, if the above mentioned assumptions are valid, it follows that 2.3…”
Section: Comparison With Experimental Data and Discussionmentioning
confidence: 98%
“…Eight separate measurements were made at each composition and CJ ranged from 5 mV in the water-rich solutions to 10 mV in pure DMSO although at one composition (50 wt. x) it reached 15 mV. If it is assumed that these results are equal to the standard real potentials of transfer of Ag+, then they can be combined with data obtained [33][34][35] for the solubility product of AgCl in these mixtures in order to calculate the real potential of transfer of chloride ion. It is this quantity which is shown in fig.…”
Section: Dimethyl Sulrhoxide + Water Mixturesmentioning
confidence: 99%