Biradical states of oxygen-vacancy defects in α-quartz

R. I. Mashkovtsev, D. F. Howarth, and J. A. Weil
Phys. Rev. B 76, 214114 – Published 21 December 2007

Abstract

Several radiation defects with effective electron spin S=1 have been observed in synthetic α-quartz, using room-temperature (RT) electron paramagnetic resonance (EPR) spectroscopy. It turns out that these defects had better be considered as biradicals, i.e., pairs of S=12 species. The parameter matrices g1, g2, D as well as matrices A describing the hyperfine interactions with two slightly inequivalent Si29 nuclei have been determined for the most intense (but RT unstable) such defect, which herein is labeled E1. The triplet-state approach and the biradical approach are compared. Inter-electron distances have been estimated using magnetic dipole concepts. A structure for center E1 is proposed, suggesting an oxygen (O0) vacancy with two unpaired electrons (holes) existing at silicon cations on opposite sides of the cavity, and the model is compared with the observed data and with published results for related single-unpaired electron species. Firm correlations between spin-Hamiltonian parameter matrix principal axes (EPR data) and crystallographic directions (x-ray diffraction data) have been attained.

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  • Received 31 July 2007
  • Accepted 16 October 2007

DOI:https://doi.org/10.1103/PhysRevB.76.214114

©2007 American Physical Society

Authors & Affiliations

R. I. Mashkovtsev*

  • Institute of Geology and Mineralogy, SB RAS, 630090 Novosibirsk, Russia

D. F. Howarth and J. A. Weil

  • Department of Chemistry, University of Saskatchewan, Saskatoon, Saskatchewan, Canada S7N 5C9

  • *rim@uiggm.nsc.ru
  • john.weil@usask.ca

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Vol. 76, Iss. 21 — 1 December 2007

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