1985•Journal of Physics C Solid State PhysicsOpen access

X-ray emission bands and electronic structure of crystalline and vitreous silica (SiO2)

GERHARD WIECH, Ernst Z. Kurmaev

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Abstract

The authors report measurements of the silicon X-ray K emission bands of the crystalline polymorphs of silica (SiO 2 ): alpha -quartz, beta -cristobalite, beta -tridymite, coesite (all having 4:2 coordination), stishovite (6:3 coordination) and of the vitreous forms Infrasil and Suprasil (a-SiO 2 ). For alpha -quartz and coesite the Si L 2,3 -emission bands are also presented. The K spectra of the various polymorphs of 4:2-coordinated silica exhibit small but distinct differences; the L spectra are virtually identical. The spectra are discussed along with available calculations of the electronic structure of alpha -quartz, beta -cristobalite and a-SiO 2 . While for alpha -quartz and a-SiO 2 reasonable overall agreement with the theoretical results is found, the calculated width of the gap between the bonding and non-bonding valence bands in beta -cristobalite is incompatible with experiment.

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The authors report measurements of the silicon X-ray K emission bands of the crystalline polymorphs of silica (SiO 2 ): alpha -quartz, beta -cristobalite, beta -tridymite, coesite (all having 4:2 coordination), stishovite (6:3 coordination) and of the vitreous forms Infrasil and Suprasil (a-SiO 2 ). For alpha -quartz and coesite the Si L 2,3 -emission bands are also presented. The K spectra of the various polymorphs of 4:2-coordinated silica exhibit small but distinct differences; the L spectra are virtually identical. The spectra are discussed along with available calculations of the electronic structure of alpha -quartz, beta -cristobalite and a-SiO 2 . While for alpha -quartz and a-SiO 2 reasonable overall agreement with the theoretical results is found, the calculated width of the gap between the bonding and non-bonding valence bands in beta -cristobalite is incompatible with experiment.

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Available abstract

The authors report measurements of the silicon X-ray K emission bands of the crystalline polymorphs of silica (SiO 2 ): alpha -quartz, beta -cristobalite, beta -tridymite, coesite (all having 4:2 coordination), stishovite (6:3 coordination) and of the vitreous forms Infrasil and Suprasil (a-SiO 2 ). For alpha -quartz and coesite the Si L 2,3 -emission bands are also presented. The K spectra of the various polymorphs of 4:2-coordinated silica exhibit small but distinct differences; the L spectra are virtually identical. The spectra are discussed along with available calculations of the electronic structure of alpha -quartz, beta -cristobalite and a-SiO 2 . While for alpha -quartz and a-SiO 2 reasonable overall agreement with the theoretical results is found, the calculated width of the gap between the bonding and non-bonding valence bands in beta -cristobalite is incompatible with experiment.

Key concepts: Stishovite, Tridymite, Coesite, Cristobalite, Quartz, Crystallography, Spectral line, Valence (chemistry)

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