Vibrational properties of OH groups associated with divalent cations in corundum (α-Al2O3)

被引:3
|
作者
Jollands, Michael C. [1 ]
Jin, Shiyun [2 ]
Curti, Martial [3 ]
Guillaumet, Maxime [4 ]
Beneut, Keevin [4 ]
Giura, Paola [4 ]
Balan, Etienne [4 ]
机构
[1] Gemol Inst Amer, 50 W 47th St, New York, NY 10036 USA
[2] Gemol Inst Amer, 5355 Armada Dr, Carlsbad, CA 92008 USA
[3] Bellerophon Gemlab SAS, 16 Pl Vendome, F-75001 Paris, France
[4] Sorbonne Univ, Inst Mineral Phys Mat & Cosmochim IMPMC, CNRS, MNHN,IRD, 4 Pl Jussieu, F-75252 Paris 05, France
关键词
THEORETICAL INFRARED-SPECTRA; COBALT IONS; HYDROGEN; DEFECTS; CRYSTAL; COLOR;
D O I
10.5194/ejm-35-873-2023
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The infrared spectra of synthetic corundum (alpha-Al2O3) samples either doped directly with divalent cations (Mg2+) or containing divalent cations formed by reduction of trivalent cations in H-2 gas (Co2+, Ni2+) may display broad OH stretching bands at similar to 3000 cm(-1) due to the structural incorporation of trace amounts of hydrogen. Experimental spectra recorded from some natural sapphires display a similar absorption band associated with a dominant absorption at 3161 cm(-1), and some beryllium-diffused corundum crystals show a band at 3060 cm(-1). All of these also display smaller and generally narrower bands between 1900 and 2700 cm(-1), whose natures are poorly defined. In this work, the atomic-scale structure, relative stability and infrared spectroscopic properties of a series of OH defects in corundum (alpha-Al2O3) are theoretically investigated at the density-functional-theory level. The investigated defects consist of interstitial H+ ions forming OH groups and compensating for the charge imbalance related to the presence of divalent cations (Be2+, Mg2+, Cr2+, Mn2+, Fe2+, Co2+, Ni2+) substituted for Al3+ at nearby octahedral sites. Bands occurring at similar to 3000 cm(-1) in experimental spectra are assigned to the OH stretching modes of some of these defects, with bands observed around 1900 and 2700 cm(-1) being assigned to overtones of corresponding OH bending modes. The results also support the assignment of the so-called "3161 cm(-1) series", observed in experimental spectra of some rubies and yellow sapphires, to structural OH groups in association with Fe2+ ions, rather than Si4+, as has been previously proposed. These inferences are also supported by analysis of correlations between band areas in experimental infrared spectra extracted from a database of corundum gemstones. A qualitative explanation relating the anomalous intensity and the polarisation properties of the OH bending overtone bands to the electrical anharmonicity of OH groups involved in medium-strength H bonds is proposed.
引用
收藏
页码:873 / 890
页数:18
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