An X-ray absorption spectroscopy study of the structure and reversibility of copper adsorbed to montmorillonite clay

Citation
Jd. Morton et al., An X-ray absorption spectroscopy study of the structure and reversibility of copper adsorbed to montmorillonite clay, GEOCH COS A, 65(16), 2001, pp. 2709-2722
Citations number
50
Categorie Soggetti
Earth Sciences
Journal title
GEOCHIMICA ET COSMOCHIMICA ACTA
ISSN journal
00167037 → ACNP
Volume
65
Issue
16
Year of publication
2001
Pages
2709 - 2722
Database
ISI
SICI code
0016-7037(200108)65:16<2709:AXASSO>2.0.ZU;2-I
Abstract
X-ray absorption spectroscopy (XAS) and adsorption-desorption measurements have been performed to assess the relationship between the structure and re versibility of copper complexes on montmorillonite clay. By varying the sol ution pH and background electrolyte concentration, the adsorption of copper on either the edge sites or permanent charge sites of montmorillonite was controlled. This allowed the structure and reversibility of copper complexe s on each of these site types to be assessed independently of each other. X AS analysis of copper adsorbed on the permanent charge sites indicated oute r-sphere surface complexes, with these complexes showing sorption reversibi lity. For copper complexes formed on the edge sites of montmorillonite, XAS data confirmed the presence of monomer and dimer copper surface complexes. Sorption irreversibility at edge sites was noted at copper coverages less than 20 mu moles/g clay at pH=4.2 and at coverages greater than 50 mu moles /g clay at pH=6.8. At pH=6.8, higher Cu-Cu coordination numbers indicated t he copper sorption irreversibility may be due, in part, to the formation of dimer surface complexes. The coordination numbers at pH=4.2 indicated the irreversibility could be due to the formation of dimers or due to formation of surface complexes on high energy edge sites. Copyright (C) 2001 Elsevie r Science Ltd.