| 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 |