A report appearing in 1975 demonstrated that incompletely out-gassed, powdered titanium dioxide photo-reduces acetylene to ethylene and prompted attempts to achieve the photoreduction of molecular nitrogen under similar conditions. Whereas pure, powdered anatase was only slightly active, a substantial enhancement of its photocatalytic activity was achieved by impregnating it with a small percentage of iron, causing its partial conversion to rutile by a heat-treatment at 1000°C. After humidification, this TiO2 substratum, on exposure to light in an argon atmosphere, exhibited activity in the water-splitting reaction and yielded NH3 in the presence of molecular nitrogen. Subsequent studies demonstrated that this N2 photoreduction occurs in a stepwise fashion via diazene and hydrazine as the intermediates. These reactions were shown to take place under simulated terrestrial conditions on the surface of rutile-containing minerals on exposure to sunlight. Evidence for the secondary photoxidation of NH3 on rutile-containing minerals was also obtained. In view of the wide distribution of titanium minerals on the Earth's crust, these abiological, light-driven reactions contribute to the nitrogen ecology in semiarid regions of the Earth and have been suggested to occur on the surface of Mars.
CITATION STYLE
Schrauzer, G. N. (2011). Photoreduction of Nitrogen on TiO2 and TiO2-Containing Minerals. Green Energy and Technology, 33, 601–623. https://doi.org/10.1007/978-0-85729-638-2_18
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