Origin of Ultrasonic Absorption in Heavy Water
- 5 October 1969
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 186 (1) , 105-107
- https://doi.org/10.1103/physrev.186.105
Abstract
Hall's theory of structural relaxation is applied to explain the excess ultrasonic absorption in O. Two states, one characterized by higher volume and lower energy (icelike structure) and the other characterized by lower volume and higher energy (close-packed structure) are assumed to be available to each molecule of O. The occurrence of a density maximum at 11.2°C and a static compressibility minimum at about 75°C favors a two-state model for O. The absorption coefficient is calculated with three trial values of (16×, 17×, and 18× /dyn). It is found that with /dyn, Hall's theory agrees very well with the experimental results.
Keywords
This publication has 3 references indexed in Scilit:
- Temperature Variation of Velocity and Absorption Coefficient of Ultrasonic Waves in Heavy Water (D2O)The Journal of the Acoustical Society of America, 1953
- Density of Heavy WaterNature, 1949
- The Origin of Ultrasonic Absorption in WaterPhysical Review B, 1948