Computer Science
Scientific paper
Aug 1997
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997gecoa..61.3041p&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 61, Issue 15, pp.3041-3049
Computer Science
4
Scientific paper
We demonstrate, using dynamic 17 O-NMR spectroscopy, that fluoride ions in the inner-coordination sphere of AlF x (H 2 O) 6-x 3-x (aq) complexes (0 x 2) progressively enhance, by orders of magnitude, the rate of exchange of waters from the innersphere to the bulk solvent. At 298K, the rate of the elementary ligand-exchange reaction increased approximately linearly with each fluoride substitution from about 2 s -1 for the fully hydrated [Al(H 2 O) 6 3+ (aq)] complex to about 2 × 10 4 s -1 for the difluoro [AlF 2 (H 2 O) 4 + (aq)] complex. A similar effect can be expected for isoelectronic complexes, such as the hydrolysis product: AlOH(H 2 O) 5 2+ (aq). By hypothesis, a similar phenomenon accounts for fluoride-enhanced release of metals from a dissolving mineral surface. If so, it should be possible to predict the effectiveness of different adsorbed ligands to enhance dissolution of minerals from spectroscopic rate measurements on dissolved complexes, as was recently shown for aminocarboxylate ligands and NiO(s) (Ludwig et al., 1995, 1996).
Casey William H.
Neugebauer Crawford Susan
Phillips Brian L.
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