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
Electron Density Study of Garnets: Y3X2Al3O12;X=Al andX=(Al, Cr)
β Scribed by Haruo Sawada
- Publisher
- Elsevier Science
- Year
- 1997
- Tongue
- English
- Weight
- 380 KB
- Volume
- 134
- Category
- Article
- ISSN
- 0022-4596
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β¦ Synopsis
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 height extending between the octahedral Al site and the coordinated oxygen atoms. YCG shows residuals around the Y and oxygen sites indicating significant anharmonicity, along with electron density deformation of the X-site characteristic of octahedral Cr 3Ψ sites. Partial substitution of Al by Cr in the X site does not increase the unshared O-O distance or the far Y-O distance in the adjacent Y site. [Cubic Ia3 d, Z β«Ψβ¬ 8. For YAG, a β«Ψβ¬ 12.0095(4) A s ; D x β«Ψβ¬ 4.553 g/cm 3 ;
π SIMILAR VOLUMES
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