Abstract
The heat capacity of α-quartz has been computed over the temperature range 10–700°K, and that of vitreous silica from 10° to 900°K. Debye θ's obtained from the T3 law below 10° were used for the ``translational'' degrees of freedom, and recent infrared and Raman data for the other frequencies. Cp—Cv was negligible for vitreous silica and was computed from compressibility and thermal-expansion data for α-quartz. Agreement with new Cp measurements is excellent for α-quartz (within 1% above 60°K) but is less satisfactory for vitreous silica because of inadequate knowledge of the distribution of frequencies below 500 cm—1.
References
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Dates
Type | When |
---|---|
Created | 20 years, 7 months ago (Jan. 5, 2005, 8:40 p.m.) |
Deposited | 1 year, 6 months ago (Feb. 8, 2024, 12:57 p.m.) |
Indexed | 1 month ago (July 20, 2025, 12:01 a.m.) |
Issued | 68 years, 6 months ago (Feb. 1, 1957) |
Published | 68 years, 6 months ago (Feb. 1, 1957) |
Published Print | 68 years, 6 months ago (Feb. 1, 1957) |
@article{Lord_1957, title={Calculation of the Heat Capacity of α Quartz and Vitreous Silica from Spectroscopic Data}, volume={26}, ISSN={1089-7690}, url={http://dx.doi.org/10.1063/1.1743274}, DOI={10.1063/1.1743274}, number={2}, journal={The Journal of Chemical Physics}, publisher={AIP Publishing}, author={Lord, R. C. and Morrow, J. C.}, year={1957}, month=feb, pages={230–232} }