Aluminium-27 n.m.r. studies of aluminium fluoro complexes in dichloromethane solution: evidence for tetrafluoroaluminate anion
Creators
- 1. Melbourne Univ., Parkville (Australia). Dept. of Inorganic Chemistry
Description
Mixed aluminium chloro/fluoro anions are formed in dichloromethane solution by the interaction of AlCl3 and [Ph3PhCH2P] [H2F3]. Aluminium-27 n.m.r. studies are restricted to the stoichiometric ranges F/Al from 1:1 to 3:1 and F/Al>8:1. Between these limits rapid precipitation reactions occur. In the fluoride-rich stoichiometric range there is rapid exchange on the n.m.r. time scale between the aluminium fluoro anion and free fluoride, so that a direct identification of the species by the multiplicity of the resonance is not possible. Indirect evidence strongly suggests that the aluminium species is [AlF4]-. In the F/Al stoichiometry range from 1:1 to 3:1 aluminium-27 resonances were observed for all the other possible [AlClχF4-χ]- species. Studies on the aluminium iodo/fluoro system support the identification of [AlF4]-, but the system is labile and the mixed iodo/fluoro species undergo rapid disproportionation. 12 refs., 1 fig
Additional details
Publishing Information
- Journal Title
- Australian Journal of Chemistry
- Journal Volume
- 42
- Journal Issue
- 9
- Series
- Aust. J. Chem.
- Journal Page Range
- 1605-1609
- ISSN
- 0004-9425
- CODEN
- AJCHA
INIS
- Country of Publication
- Australia
- Country of Input or Organization
- Australia
- INIS RN
- 21017682
- Subject category
- S37: INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY;
- Descriptors DEI
- ALUMINIUM CHLORIDES; ALUMINIUM COMPLEXES; ALUMINIUM FLUORIDES; ALUMINIUM 27; CHEMICAL SHIFT; METHYLENE CHLORIDE; NMR SPECTRA; NONAQUEOUS SOLVENTS
- Descriptors DEC
- ALUMINIUM COMPOUNDS; ALUMINIUM ISOTOPES; CHLORIDES; CHLORINE COMPOUNDS; COMPLEXES; FLUORIDES; FLUORINE COMPOUNDS; HALIDES; HALOGEN COMPOUNDS; ISOTOPES; LIGHT NUCLEI; NUCLEI; ODD-EVEN NUCLEI; ORGANIC CHLORINE COMPOUNDS; ORGANIC COMPOUNDS; ORGANIC HALOGEN COMPOUNDS; SOLVENTS; SPECTRA; STABLE ISOTOPES