Physical properties of oxygen-17 water. Absolute viscosity and density of H217O between 15 and 35°C

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dc.contributor.authorKudish, Albert I.
dc.contributor.authorWolf, David
dc.contributor.authorSteckel, Fritz
dc.date.accessioned2025-02-15T04:49:30Z
dc.date.available2025-02-15T04:49:30Z
dc.date.issued1974
dc.description.abstractThe absolute viscosity of four oxygen-17 water samples is reported at 5°C intervals between 15 and 35°C. The absolute viscosity of 100 % H217O is determined by extrapolation of the measured viscosity of a highly enriched oxygen-17 sample, i.e., 86.53 %17O. The values calculated, based upon Eyring's theory of viscosity, for the other oxygen-17 samples are in excellent agreement with the experimental results. The isotope effect has been analyzed for H217O relative to natural water. The viscosity ratio at 25°C for H217O/H216O is 1.0226, whereas that for H218O/H216O and D216O/H216O is 1.0536 and 1.2316, respectively.en_US
dc.identifier.urihttp://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/17746
dc.language.isoenen_US
dc.publisherJournal of the Chemical Society : Faraday Transaction - I. The Chemical Society, London. 1974, 70 (1-6)en_US
dc.subjectChemistryen_US
dc.subjectIsotopic Wateren_US
dc.subjectThermophysical Propertiesen_US
dc.subjectJournal of the Chemical Society : Faraday Transaction - Ien_US
dc.titlePhysical properties of oxygen-17 water. Absolute viscosity and density of H217O between 15 and 35°Cen_US
dc.typeArticleen_US

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