Physical Properties of Heavy-oxygen Water:  Absolute Viscosity of H218O between 15 and 35°C

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DC Field	Value	Language
dc.contributor.author	Kudish, A. I.	-
dc.contributor.author	Wolf, D.	-
dc.contributor.author	Steckel, F.	-
dc.date.accessioned	2025-02-03T06:41:42Z	-
dc.date.available	2025-02-03T06:41:42Z	-
dc.date.issued	1972	-
dc.identifier.uri	http://dspace.bits-pilani.ac.in:8080/jspui/handle/123456789/17033	-
dc.description.abstract	The absolute viscosity of highly enriched heavy-oxygen water, H218O, has been measured at 5°C intervals between 15 and 35°C, using a semi-automatic closed viscometer of the suspended-level type. A linear extrapolation was performed to determine the viscosity of 100 % heavy-oxygen water, based upon the measured viscosity of natural water and that of a highly enriched heavy-oxygen water sample. The effect of isotope substitution on the viscosity of natural water has been analyzed for both H218O and D216O. The viscosity ratio at 25°C for H218O/H216O is 1.0536, whereas that for D216O/H216O is 1.2316.	en_US
dc.language.iso	en	en_US
dc.publisher	Journal of the Chemical Society : Faraday Transaction - I. The Chemical Society, London. 1972, 68 (11)	en_US
dc.subject	Chemistry	en_US
dc.subject	Heavy-Oxygen Water	en_US
dc.subject	H₂¹⁸O	en_US
dc.subject	Absolute Viscosity	en_US
dc.subject	Temperature Dependence	en_US
dc.subject	Journal of the Chemical Society : Faraday Transaction - I	en_US
dc.title	Physical Properties of Heavy-oxygen Water: Absolute Viscosity of H218O between 15 and 35°C	en_US
dc.type	Article	en_US
Appears in Collections:	Journal Articles (before-1995)

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