Research output: Contribution to Journal/Magazine › Journal article › peer-review
<mark>Journal publication date</mark> | 29/06/1993 |
---|---|
<mark>Journal</mark> | Colloids and Surfaces A: Physicochemical and Engineering Aspects |
Volume | 73 |
Number of pages | 19 |
Pages (from-to) | 145-163 |
Publication Status | Published |
<mark>Original language</mark> | English |
Aqueous dispersions of colloidal hematite were prepared by aqueous precipitation and characterised using X-ray diffraction and Fourier transform infrared spectroscopy. Their surface chemistry was studied using (photo-)electrophoresis, in which electrophoretic mobilities were determined by laser Doppler electrophoresis, in the absence and presence of irradiation of photons from a xenon lamp and monochromator. Absorption of ultra-band-gap energy photons in Fe2O3 results in the generation of electron (e-)-hole (h+) pairs, which may then recombine, with the generation of heat/radiation, or react with lattice sites, solvent or solution species.
Changing the pH of alpha-Fe2O3 particle preparation from 2 to 1.4 was found to alter the resultant surface from one comprising mostly alpha-Fe2O3, alpha-FeOOH and gamma-FeOOH with an isoelectric point (i.e.p.) of 7.4, to one whose behaviour was dominated by the presence of delta-FeOOH with an i.e.p. of 1.5. The alpha-Fe2O3 particles whose surfaces are found to be mostly ''Fe(OH)3''/Fe2O3.nH2O in character exhibit a continuum of i.e.p.s due to the non-crystalline nature of that phase. Large changes in the electrophoretic mobility of colloidal alpha-Fe2O3 at a pH of less than about 7-8 were observed upon irradiation with photons with ultra-band-gap energies, indicative of the formation of net surface positive charge, due to the hole-driven photo-oxidation of surface >Fe-OH sites to form (>Fe-OH)+ sites. Photogenerated conduction band electrons were removed from the particles via either the reductive dissolution of the alpha-Fe2O3 surface or, possibly, the formation of hydrogen from the reduction of H+ ions. The photoelectrophoretic mobility-illumination wavelength spectrum of colloidal alpha-Fe2O3 exhibits two distinct mobility change onsets, one at 2.2 eV and the other at 3 eV, reflecting the presence of an ''upper'' and ''lower'' valence band on hematite. The oxidation of surface >Fe-OH groups responsible for the change in net surface positive charge is found to proceed ten times more slowly than the corresponding reaction on colloidal TiO2.