Abstract
The absolute viscosity of highly enriched heavy-oxygen water, H 218O, 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 H 218O and D216O. The viscosity ratio at 25°C for H218O/H216O is 1.0536, whereas that for D216O/H216O is 1.2316.
| Original language | English |
|---|---|
| Pages (from-to) | 2041-2046 |
| Number of pages | 6 |
| Journal | Physical Chemistry Chemical Physics |
| Volume | 68 |
| DOIs | |
| State | Published - 1 Dec 1972 |
| Externally published | Yes |
ASJC Scopus subject areas
- General Chemistry