The crystal structures of seven crystals from five garnet mineral species have been studied through single-crystal X-ray diffraction methods incorporating scattering factor refinement procedures. The derived experimental scattering factors for each atomic species show similar scattering-angle-depend
Electron Density Study of Garnets: Ca3(Cr, Al)2Si3O12
β Scribed by Haruo Sawada
- Publisher
- Elsevier Science
- Year
- 1997
- Tongue
- English
- Weight
- 223 KB
- Volume
- 132
- Category
- Article
- ISSN
- 0022-4596
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β¦ Synopsis
The electron density distribution in a natural garnet, uvarovite Ca 3 (Cr, Al) 2 Si 3 O 12 with 55% of the octahedral site occupied by Cr, has been studied with single-crystal X-ray diffraction methods through scattering factor refinement procedures. Electron density residuals up to 0.22 e/A s 3 in height indicating bonding electrons were detected between Si and oxygen. Characteristic aspherical electron density distribution around the (Cr, Al) site was also seen; six residuals, Ψ0.27 e/A s 3 in height, are directed toward the coordinated oxygens, eight with 0.15 e/A s 3 height are directed away from the oxygens. [Cubic Ia3 d, a β«Ψβ¬ 11.956(1)A s ;
π SIMILAR VOLUMES
The electron density distribution in two garnets Y 3 Al 2 Al 3 O 12 [YAG] and Y 3 X 2 Al 3 O 12 : X β«Ψβ¬ (Al 0.71 Cr 0.29 ) [YCG] have been studied with single-crystal X-ray diffraction methods through scattering factor refinement procedures. YAG has broad electron density residuals of 0.3 e/A s 3 he
The electron density distribution in garnets, Z 3 Ga 5 O 12 , Z β«Ψβ¬ Nd, Sm, Gd, Tb, has been studied with single-crystal X-ray diffraction methods through scattering factor refinement procedures. The Z site shows a variety of electron density residual distribution modes, implying contribution of the
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