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 |