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Please use this identifier to cite or link to this item: http://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/20187
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dc.contributor.authorFeakins, David-
dc.contributor.authorO’Shaughnessy, Denis A.-
dc.date.accessioned2025-11-21T13:54:32Z-
dc.date.available2025-11-21T13:54:32Z-
dc.date.issued1978-
dc.identifier.urihttp://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/20187-
dc.description.abstractWashburn numbers for alkali-metal chlorides have been measured in the range 0-40 % (w/w) DMSO (x2 = 0-0.094) and are compared with literature values for H+CI-. There is evidence for significant incorporation of DMSO into near-neighbour shells of H+ and Li+; by making certain assumptions it is concluded that these ions, and Cl-, are preferentially solvated by DMSO. The Washburn numbers of H+Cl, LrCl- and K+Cl- show maxima when plotted against ,v2. Possible explanations of this behaviour, which is paralleled by that of the Walden products, are discussed in detail, and it is concluded that it arises mainly from shifts in the preferential rather than the total solvation of the ions. The maxima in are evidence for the retention of water-like structure in the region studied, but not necessarily for its enhancement.en_US
dc.language.isoenen_US
dc.publisherJournal of the Chemical Society : Faraday Transaction - I. The Chemical Society, London. 1978, 74 (02)en_US
dc.subjectJournal of the Chemical Society : Faraday Transaction - Ien_US
dc.subjectChemistryen_US
dc.subjectWashburn Numbersen_US
dc.subjectAlkali-metal Chloridesen_US
dc.titleWashburn Numbers: Part 3.—Alkali-metal Chlorides in the DMSO4-Water System; Comparison with Hydrochloric Acid ; “ Structural ” Effectsen_US
dc.typeArticleen_US
Appears in Collections:Journal Articles (before-1995)

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