Redox state and mobility of iron at the asbestos surface: a voltammetric approach

Citation
L. Prandi et al., Redox state and mobility of iron at the asbestos surface: a voltammetric approach, J MAT CHEM, 11(5), 2001, pp. 1495-1501
Citations number
27
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science","Material Science & Engineering
Journal title
JOURNAL OF MATERIALS CHEMISTRY
ISSN journal
09599428 → ACNP
Volume
11
Issue
5
Year of publication
2001
Pages
1495 - 1501
Database
ISI
SICI code
0959-9428(2001)11:5<1495:RSAMOI>2.0.ZU;2-N
Abstract
The mechanism by which asbestos causes the development of cancer in people exposed to airborne fibres, still unclear at the molecular level, seems to involve iron ions located at particular sites at the fibre surface. In this paper, cyclic voltammetry has been employed to investigate the oxidation s tate and mobility of iron ions on crocidolite and amosite, the two most com mon types of amphibole asbestos. Experiments have been carried out at three pH values: 0.5, at which iron is spontaneously released from the solids; n eutral (close to the extracellular and cytoplasmatic value); and 4.5, repre sentative of the lysosomial fluid, i.e. of the environment to which a phago cytized fibre is exposed. An Fe-exchanged Y zeolite and an Fe-silicalite ha ve been used for comparison as 'model solids'. At neutral pH iron is readil y mobilised from FeY upon cycling, in contrast with Fe-silicalite. With bot h asbestos materials, at neutral pH iron is mobilised during the subsequent cycles and is brought into solution, amosite releasing more iron than croc idolite per unit area under the same conditions. Three couples of redox pea ks are seen, centred at ca. 0.0, -0.2 and +0.6 V. The first is due to the F e3+/Fe2+ couple in solution, the second is probably related to the Fe3+/Fe2 + at the surface of the asbestos particle, and the third is assigned to sur face iron in an oxidation state higher than three. At pH 0.5, the couple of peaks due to surface Fe is absent and mobilisation immediately occurs. The release of iron at pH 0.5 from asbestos was also measured photometrically and, in the first two hours, corresponds to that expected for the outermost layer of the minerals. Voltammetric cycling markedly enhances the amount o f Fe solubilised. Partial oxidation or reduction of surface iron ions was o btained by keeping the sample at a defined potential before cycling: subseq uent voltammograms indicate that the smaller Fe3+ cation is the mobilised s pecies.