Abstract
The attenuation of Rayleigh waves in quartz was measured as a function of temperature from 4.2 to 100 °K and frequency from 300 to 2000 MHz. Below 20 °K, the attenuation was observed temperature-independent. From 20 to 40 °K, the results were consistent with a three-phonon interaction process varying as T4 but with little or no dependence on frequency. Above 40 °K, the attenuation showed a lower dependence on temperature than T4 and oscillated due to an interference effect between the Rayleigh wave and a bulk wave generated at the same time.
References
4
Referenced
6
10.1103/PhysRev.173.881
/ Phys. Rev. (1968)10.1016/0041-624X(64)90228-8
/ Ultrasonics (1964)10.1063/1.1708074
/ J. Appl. Phys. (1966)10.1063/1.1652438
/ Appl. Phys. Letters (1968)
Dates
Type | When |
---|---|
Created | 21 years, 6 months ago (Feb. 3, 2004, 11:16 a.m.) |
Deposited | 1 year, 6 months ago (Feb. 5, 2024, 2:05 a.m.) |
Indexed | 1 year, 6 months ago (Feb. 5, 2024, 2:55 a.m.) |
Issued | 55 years, 7 months ago (Jan. 1, 1970) |
Published | 55 years, 7 months ago (Jan. 1, 1970) |
Published Print | 55 years, 7 months ago (Jan. 1, 1970) |
@article{Daniel_1970, title={TEMPERATURE-DEPENDENT ATTENUATION OF ULTRASONIC SURFACE WAVES IN QUARTZ}, volume={16}, ISSN={1077-3118}, url={http://dx.doi.org/10.1063/1.1653020}, DOI={10.1063/1.1653020}, number={1}, journal={Applied Physics Letters}, publisher={AIP Publishing}, author={Daniel, M. R. and de Klerk, J.}, year={1970}, month=jan, pages={30–31} }