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

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dc.contributor.author Kudish, Albert I.
dc.contributor.author Wolf, David
dc.contributor.author Steckel, Fritz
dc.date.accessioned 2025-02-15T04:49:30Z
dc.date.available 2025-02-15T04:49:30Z
dc.date.issued 1974
dc.identifier.uri http://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/17746
dc.description.abstract The 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.language.iso en en_US
dc.publisher Journal of the Chemical Society : Faraday Transaction - I. The Chemical Society, London. 1974, 70 (1-6) en_US
dc.subject Chemistry en_US
dc.subject Isotopic Water en_US
dc.subject Thermophysical Properties en_US
dc.subject Journal of the Chemical Society : Faraday Transaction - I en_US
dc.title Physical properties of oxygen-17 water. Absolute viscosity and density of H217O between 15 and 35°C en_US
dc.type Article en_US


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