Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4699972 | Chemical Geology | 2010 | 21 Pages |
Abstract
Quantum chemical calculations were combined with acid/base titrations and 13C NMR experiments to determine the structures, Gibbs free energy changes, vibrational frequencies and NMR chemical shifts characterizing the interactions of H+, Mg2+, Ca2+, Cd2+ and UO22+ with the carboxyl group of the 2-Keto-3-deoxyoctanoate (Kdo) and galacturonate molecules as models for reactive sites on bacterial surfaces. Monodentate, bidentate and outer-sphere complexation modes were considered. Results are also consistent with previous experimental and theoretical work on metal-carboxyl complexation, in particular with EXAFS studies. Among the four metals considered here, the theoretical results suggest that Mg2+ complexation is most thermodynamically favorable and UO22+ complexation is least favorable. On the other hand, our NMR experimental results suggested that Cd2+ complexation is the most favorable, whereas Mg2+ and Ca2+ complexation are weak processes, hindered by competition with H+. Apart from this discrepancy, there was a reasonable agreement between the theoretical and experimental results, which, taken together, also indicated that outer-sphere complexation was the dominant mode of complexation in our systems.
Keywords
Related Topics
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Authors
P. Selvarengan, J.D. Kubicki, J.-P. Guégan, X. Châtellier,