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Co2+-doped diopside: crystal structure and optical properties.

Authors :
Gori, C.
Tribaudino, M.
Mezzadri, F.
Skogby, H.
Hålenius, U.
Source :
Physics & Chemistry of Minerals; May2018, Vol. 45 Issue 5, p443-461, 19p
Publication Year :
2018

Abstract

Synthetic clinopyroxenes along the CaMgSi<subscript>2</subscript>O<subscript>6</subscript>-CaCoSi<subscript>2</subscript>O<subscript>6</subscript> join were investigated by a combined chemical-structural-spectroscopic approach. Single crystals were synthesized by flux growth methods, both from Ca-saturated and Ca-deficient starting compositions. Single crystal structure refinements show that the incorporation of Co<superscript>2+</superscript> at the octahedrally coordinated cation sites of diopside, increases the unit-cell as well as the M1 and the M2 polyhedral volumes. Spectroscopic investigations (UV-VIS-NIR) of the Ca-rich samples reveal three main optical absorption bands, i.e. <superscript>4</superscript>T<subscript>1g</subscript> → <superscript>4</superscript>T<subscript>2g</subscript>(F), <superscript>4</superscript>T<subscript>1g</subscript> → <superscript>4</superscript>A<subscript>2g</subscript>(F) and <superscript>4</superscript>T<subscript>1g</subscript> → <superscript>4</superscript>T<subscript>1g</subscript>(P) as expected for Co<superscript>2+</superscript> at a six-coordinated site. The bands arising from the <superscript>4</superscript>T<subscript>1g</subscript> → <superscript>4</superscript>T<subscript>2g</subscript>(F) and the <superscript>4</superscript>T<subscript>1g</subscript> → <superscript>4</superscript>T<subscript>1g</subscript>(P) electronic transitions, are each split into two components, due to the distortions of the M1 polyhedron from ideal O<subscript>h</subscript>-symmetry. In spectra of both types, a band in the NIR range at ca 5000 cm<superscript>−1</superscript> is caused by the <superscript>4</superscript>A<subscript>2g</subscript> → <superscript>4</superscript>T<subscript>1g</subscript>(F) electronic transition in Co<superscript>2+</superscript> in a cubic field in the M2 site. Furthermore, an additional component to a band system at 14,000 cm<superscript>−1</superscript>, due to electronic transitions in Co<superscript>2+</superscript> at the M2 site, is recorded in absorption spectra of Ca-deficient samples. No variations in Dq and Racah B parameters for Co<superscript>2+</superscript> at the M1 site in response to compositional changes, were demonstrated, suggesting complete relaxation of the M1 polyhedron within the CaMgSi<subscript>2</subscript>O<subscript>6</subscript>-CaCoSi<subscript>2</subscript>O<subscript>6</subscript> solid solution. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
03421791
Volume :
45
Issue :
5
Database :
Complementary Index
Journal :
Physics & Chemistry of Minerals
Publication Type :
Academic Journal
Accession number :
129685776
Full Text :
https://doi.org/10.1007/s00269-017-0932-z