K. Ogoh et al., 2-CENTER MODEL FOR RADIATION-INDUCED ALUMINUM HOLE CENTER IN STISHOVITE, Journal of physics and chemistry of solids, 57(1), 1996, pp. 85-88
Electron spin resonance (ESR) has been measured for stishovite synthes
ized under high pressure conditions from high purity SiO2 glass or nat
ural quartz and irradiated by gamma-rays both at room temperature and
at 77 K. The prominent signal detected at 77 K has anisotropic g-facto
rs of orthorhombic symmetry, g(x) = 2.0155, g(y) = 2.0094 and g(z) = 2
.0033, and hyperfine sextets (I = 5/2) with A(x) = 0.394 mT, A(y) = 0.
372 mT and A(z) = 0.436 mT. The g-factors and the hyperfine structure
indicate that this signal is due to a two-center type hole center, O-2
(3-), associated with an aluminum atom substituted at the silicon site
in stishovite.