Raman spectroscopic study of the selenite mineral: ahlfeldite, NiSeO3·2H2O
✍ Scribed by Ray L. Frost; Eloise C. Keeffe
- Publisher
- John Wiley and Sons
- Year
- 2009
- Tongue
- English
- Weight
- 164 KB
- Volume
- 40
- Category
- Article
- ISSN
- 0377-0486
- DOI
- 10.1002/jrs.2075
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## Abstract Raman spectroscopy has been used to study the dimorphous selenite minerals chalcomenite, cobaltomenite and clinochalcomenite. Selenite minerals are characterised by the position of the symmetric stretching mode that is observed at higher wavenumbers than the anti‐symmetric stretching mo
The mineral haynesite, a uranyl selenite, has been characterised by Raman spectroscopy at 298 and 77 K. Two bands at 811.5 and 800.2 cm -1 are assigned to the symmetric stretching modes of the (UO 2 / 2+ and (SeO 3 / 2-units respectively. These values give calculated U-O bond lengths of 1.799 and/or