4.6 Article

Photocatalytic activity of non-stoichiometric ZnFe2O4 under visible light irradiation

Journal

PHYSICA SCRIPTA
Volume 89, Issue 4, Pages -

Publisher

IOP PUBLISHING LTD
DOI: 10.1088/0031-8949/89/04/044011

Keywords

zinc ferrite; photocatalyst; visible light; sol-gel combustion; photoluminescence; XPS; x-ray magnetic circular dichroism

Funding

  1. National Research Program in material sciences IMIS
  2. ERDF [2010/0204/2DP/2.1.1.2.0/10/APIA/VIAA/010, 3.2.1101.12-0027, TK114, TK117]
  3. Estonian Science Foundation [8216, 8737]
  4. Estonian Ministry of Education and Research [IUT2-25]
  5. Estonian Nanotechnology Competence Center [EU29996]

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Nanostructured zinc ferrites with different excess iron contents (ZnFe2+zO4, where z = 0.00, 0.05, 0.10 and 0.15) have been synthesized using the sol-gel auto-combustion method. The effect of excess iron on the structural, optical and visible light photocatalytic activity of zinc ferrite samples has been investigated. X-ray diffraction (XRD), x-ray photoelectron spectroscopy (XPS), x-ray magnetic circular dichroism (XMCD), Brunauer-Emmett-Teller theory, scanning electron microscopy (SEM), diffuse reflectance spectroscopy (UV-Vis) and photoluminescence spectroscopy were used to characterize the synthesized non-stoichiometric ZnFe2O4 powders. The XRD patterns demonstrated that the samples consist of single phase spinel structure with crystallite sizes of similar to 25 nm. SEM analysis indicated that the nanosized particles grow together in porous clusters with a size of several microns. The XPS and XMCD analyses revealed that the excess iron ion substitutes Zn2+ in tetrahedral sites and in octahedral sites Fe2+ can be found in addition to Fe3+, which could be created to restore the overall charge balance in the crystal lattice. Stoichiometric zinc ferrite (ZnFe2+zO4, z = 0.00) exhibited higher photocatalytic activity (40%) than the excess iron sample (ZnFe2+zO4, z = 0.15, i.e. 4%) under visible light irradiation for 3 h. This was explained by the formation of Fe2+ in the octahedral sites of excess iron ZnFe2O4; these species act as recombination centres.

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