Factors of 18O/16O fractionation in corundum estimated from the calculation of isotopic shifts on vibration frequencies
- Авторлар: Krylov D.P.1, Glebovitskii V.A.1,2, Akimova E.Y.1,2
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Мекемелер:
- Institute of Precambrian Geology and Geochronology
- Institute of Earth Sciences
- Шығарылым: Том 55, № 6 (2017)
- Беттер: 589-594
- Бөлім: Short Communications
- URL: https://journals.rcsi.science/0016-7029/article/view/155528
- DOI: https://doi.org/10.1134/S0016702917060064
- ID: 155528
Дәйексөз келтіру
Аннотация
The β-factors of corundum were estimated on the basis of DFT calculations of vibrational frequency changes due to 16O–18O isotope substitution in a harmonic approximation using an all-electron Gaussian-type basis set and the B3LYP hybrid functional (the CRYSTAL program). Calculations were performed accounting for eight phonon wave vectors within the first Brillouin zone. The results are approximated by the relation 1000ln βcrn = 9.19874x–0.12326x2 + 0.00213x3 (x = 106/T(K)2, 400 < T(K) < 1300), which can be used in isotope geochemical studies in combination with the known temperature effects on the β-factors of other phases.
Негізгі сөздер
Авторлар туралы
D. Krylov
Institute of Precambrian Geology and Geochronology
Хат алмасуға жауапты Автор.
Email: dkrylov@dk1899.spb.edu
Ресей, St. Petersburg, 199034
V. Glebovitskii
Institute of Precambrian Geology and Geochronology; Institute of Earth Sciences
Email: dkrylov@dk1899.spb.edu
Ресей, St. Petersburg, 199034; St. Petersburg, 199034
E. Akimova
Institute of Precambrian Geology and Geochronology; Institute of Earth Sciences
Email: dkrylov@dk1899.spb.edu
Ресей, St. Petersburg, 199034; St. Petersburg, 199034
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