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.