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

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DC Field	Value	Language
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
Appears in Collections:	Journal Articles (before-1995)

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