Raman spectroscopy of dimethyl sulphoxide and deuterated dimethyl sulphoxide at 298 and 77 K
✍ Scribed by Wayde N. Martens; Ray L. Frost; János Kristof; J. Theo Kloprogge
- Publisher
- John Wiley and Sons
- Year
- 2002
- Tongue
- English
- Weight
- 133 KB
- Volume
- 33
- Category
- Article
- ISSN
- 0377-0486
- DOI
- 10.1002/jrs.827
No coin nor oath required. For personal study only.
📜 SIMILAR VOLUMES
## 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
The differential pulse polarographic behaviour in dimethyl sulphoxide (DMSO) of 14 organotin(1V) compounds having the general formula R3SnX (R = Me, Ph; X-= NCS-, Ny, NO;, OH-, NCOand OAc -) and "Bu3SnCI and "Bu2SnC12 has been studied. The peak potential was found to depend markedly on the organic g
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