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Bibliographic Data:


Code: KILLS98
Paper Type: Article
Author(s): Karasyova ON, Ivanova LI, Lakshtanov LZ, Loevgren L, Sjoeberg S
Title: Complexation of Gold(III)-Chloride at the Surface of Hematite
Journal: Aquatic Geochemistry
Volume: 4   Year: 1998   Pages: 215-231
ISSN-Print: 1380-6165
Internal Storage: V835
DOI: 10.1023/A:1009622915376
Abstract:

The acid/base properties of the hematite/water interface and surfacecomplexation with gold has been studied by potentiometric titrations in thefour component system H+ – ≡FeOH –AuCl4 – Cl&minus:. Equilibrium measurementswere performed in NaCl media at 298.2 K. In the evaluation of equilibriummodel from experimental data the constant capacitance model was applied. Theacid/base properties were investigated in 0.1 M NaCl in the range 2.6 ≤ pH ≤ 7.4. The resulting intrinsic constants for protonation anddeprotonation of hydroxyl groups at the surface were logβ1,1,0,0(int)s = 7.10 ± 0.06 and logβ−1,1,0,0(int)s = −7.80 ± 0.06. The density of proton active surface sites was 2.85 nm−2 and the specific capacitance 2.5 C V−1 m−2. In the investigation of surface complexation of gold, thepotentiometric titrations were performed in the range 2.0 ≤ pH ≤ 10.2.Titration data was supplemented with analysis of Au in the aqueous phase byatomic absorbance spectrometry. The equilibrium model proposed consists ofthe following monodentate surface complexes: ≡FeOHAuCl3(log β0,1,1,−1s = 1.45 ± 0.03), ≡FeOHAuCl2OH (log β−1,1,1,−2s = −3.89 ± 0.02), ≡FeOHAu(OH)3 (log β−3,1,1,−4s = −21.94 ± 0.05). Aslightly better fit could be obtained by assuming formation of a bidentatecomplex with the composition(≡FeO)2Au(OH)H2O. However, based onstructural arguments this complex was rejected.

Comment: used log K for AuCl4- formation not reported

Surface Area   |   Site Density / Protolysis   |   Complex Formation   |   Formatted Citation