Issue 15, 2000

Photocatalytic oxygen evolution on α-Fe2O3 films using Fe3+ ion as a sacrificial oxidizing agent

Abstract

Photocatalytic oxygen evolution on α-Fe2O3 films was studied using the Fe3+ ion as a sacrificial oxidizing agent. The reaction conditions affecting the oxygen evolution rate, i.e. anion, Fe3+ concentration, pH, Fe3+/Fe2+ equilibrium concentration and dependence of irradiation wavelength, were investigated. The reaction rate increased with increase of both the Fe3+ ion concentration and the solution pH. Oxygen evolution ceased at an Fe3+ :Fe2+ ion concentration ratio of 3:7–4: 6. The reaction rate decreased rapidly for longer-wavelength irradiation (above around 400 nm), which is considerably shorter than the α-Fe2O3 bandgap of ca. 600 nm (2.1 eV).

Article information

Article type
Paper
Submitted
17 May 2000
Accepted
12 Jun 2000
First published
06 Jul 2000

Phys. Chem. Chem. Phys., 2000,2, 3519-3522

Photocatalytic oxygen evolution on α-Fe2O3 films using Fe3+ ion as a sacrificial oxidizing agent

T. Ohmori, H. Takahashi, H. Mametsuka and E. Suzuki, Phys. Chem. Chem. Phys., 2000, 2, 3519 DOI: 10.1039/B003977M

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