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Raman Spectroscopy of the Low-Frequency Region of Kaolinite at 298 and 77 K

โœ Scribed by Frost, Ray L.; Kloprogge, J. Theo

Book ID
115364290
Publisher
Society for Applied Spectroscopy
Year
1999
Tongue
English
Weight
289 KB
Volume
53
Category
Article
ISSN
0003-7028

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Raman spectra of kaolinite and of the formamide-intercalated kaolinite were obtained at both 298 and 77 K using a Raman microprobe equipped with a thermal stage. Upon cooling to 77 K, the band attributed to the inner hydroxyl shifts by 5 cm-1 to lower wavenumbers and the bands assigned to the inner

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## Abstract A comparative study of a suite of natural oxalates including weddellite, whewellite, moolooite, humboldtine, glushinskite, natroxalate and oxammite was undertaken using Raman spectroscopy at 298 and 77 K. Oxalates are found as films on host rocks as a result of heavy metal expulsion by