Hostname: page-component-586b7cd67f-t7fkt Total loading time: 0 Render date: 2024-11-24T04:08:47.975Z Has data issue: false hasContentIssue false

Antimony(V) complexing with O-bearing organic ligands in aqueous solution: an X-ray absorption fine structure spectroscopy and potentiometric study

Published online by Cambridge University Press:  05 July 2018

M. Tella*
Affiliation:
Experimental Geochemistry and Biogeochemistry Group, Laboratoire des Mécanismes et Transfert en Géologie, LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Av. E. Belin, F-31400 Toulouse, France
G. S. Pokrovski
Affiliation:
Experimental Geochemistry and Biogeochemistry Group, Laboratoire des Mécanismes et Transfert en Géologie, LMTG, Université de Toulouse, CNRS, IRD, OMP, 14 Av. E. Belin, F-31400 Toulouse, France
*

Abstract

The stabilityand structure of aqueous complexes formed by pentavalent antimony (SbV) with simple organic ligands (acetic, adipic, oxalic, citric acids, catechol and xylitol) having O-functional groups (carboxyl, alcoholic hydroxyl, aliphatic and aromatic hydroxyl) typical of natural organic matter (NOM), were determined at 25°C from potentiometric and X-ray absorption fine structure spectroscopy (XAFS) measurements. In organic-free aqueous solutions, spectroscopic data are consistent with the dominant formation of SbV hydroxide species, Sb(OH)5 and Sb(OH)6-, at acid and near-neutral to basic pH, respectively. Potentiometric measurements demonstrate negligible complexing with mono-functional organic ligands (acetic) or those having non-adjacent carboxylic groups (adipic). In contrast, in the presence of poly-functional carboxylic, hydroxyl carboxylic acids and aliphatic and phenolic hydroxyl, SbV forms stable 1:1 or 1:3 complexes in coordination 6 with the studied organic ligands, over a wide pH range pertinent to natural waters (3 ≤ pH ≤ 9). The XAFS measurements show that in these species the central SbV atom has an octahedral geometry with 6 oxygen atoms from hydroxyl moieties and adjacent functional groups (O = C—OH and/or C—OH) of the ligand, forming bidendate chelate cycles. Stability constants for SbV-oxalate complexes generated from potentiometric experiments were used to model SbV complexing with di-carboxylic functional groups of natural humic acids. Our predictions show that in an aqueous solution of pH between 1 and 4 containing 1 μg/l of Sb and 5 mg/l of dissolved organic carbon (DOC), up to 15% of total dissolved Sb maybe bound to aqueous organic matter via di-carboxylic groups.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2008

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Akinviev, N.N. (1986) BALANCE: IBM computer code for calculating mineral-aqueous solution-gas equilibria. Geochemistry, 6, 882–890.Google Scholar
Baes, C.F. and Mesmer, R.E. (1976) The Hydrolysis of Cations. Wiley.Google Scholar
Buschmann, J. and Sigg, L. (2004) Antimony(III) binding to humic substances: influence of pH and type of humic acid. Environmental Science and Technology, 38, 4535–4541.CrossRefGoogle ScholarPubMed
Filella, M., Belzile, N. and Chen, Y.-W. (2002) Antimony in the environment: a review focused on natural waters: I. Occurrence. Earth Science Reviews, 57, 125–176.CrossRefGoogle Scholar
Filella, M. and May, P.M. (2005) Critical appraisal of available thermodynamic data for the eomplexation of antimony(III) and antimony(V) by low molecular mass organic ligands. Journal of Environmental Monitoring, 7, 1226–1237.CrossRefGoogle ScholarPubMed
Linder, P.W. and Murray, K. (1987) Statistical determination of molecular structure and the metal binding sites of fulvic acids. Science of the Total Environment, 64, 149–161.CrossRefGoogle Scholar
Newville, M. (2001) IFEFFIT: interactive XAFS analysis and FEFF fitting. Journal of Synchrotron Radiation, 8, 322–324.CrossRefGoogle ScholarPubMed
Pokrovski, G.S., Borisova, A.Y., Roux, J., Hazemann, J.-L., Petdang, A., Telia, M. and Testemale, D. (2006) Antimony speciation in saline hydrothermal fluids: A combined X-ray absorption fine structure spectroscopy and solubility study. Geochimica et Cosmochimica Ada, 70, 4196–4214.CrossRefGoogle Scholar
Ravel, B. and Newville, M. (2005) Athena, Artemis, Hephaestus: data analysis for X-ray absorption spectroscopy using Ifeffit. Journal of Synchrotron Radiation, 12, 537–541.CrossRefGoogle ScholarPubMed
Steely, S., Amarasiriwardena, D. and Xing, B. (2007) An investigation of inorganic antimony species and antimony associated with soil humic acid molar mass fractions in contaminated soils. Environmental Pollution, 148, 590–598.CrossRefGoogle ScholarPubMed
Telia, M. and Pokrovski, G.S. (2008) Antimony(III) complexing with O-bearing organic ligands in aqueous solution: An X-ray absorption fine structure spectroscopy and solubility study. Geochimica et Cosmochimica Ada, (submitted).CrossRefGoogle Scholar
Thurman, E.M. (1985) Organic Geochemistry of Natural Waters. Martinus Nijhoff, Dr W. Junk Publ., Boston, USA.CrossRefGoogle Scholar