Abstract

The catalytic activity of hexaaluminate is closely related to the chemical state of substituted active metal ions. In this paper, the mechanism of stabilization of Fe ions in β I-Al 2O 3 and magnetoplumbite-type Fe-substituted Ba hexaaluminates was proposed at the molecule level on the basis of X-ray diffraction, Rietveld refinement, and Mössbauer spectroscopy. Fe 3+ ions originated from oxidic entities dispersed on Ba-modified γ-Al 2O 3 mainly entered into the sites in the loosely packed mirror plane of the hexaaluminates. In particular, Fe 3+ ions at low concentration preferentially occupied the tetrahedral Al(5) sites of the β I-Al 2O 3 phase, while Fe 3+ ions at high concentration mainly occupied the trigonal bipyramidal Al(5) and octahedral Al(3) sites in the magnetoplumbite phase. Meanwhile, tetrahedral Fe 3+ ions in the intermediate spinel-type BaAl 2O 4 phase preferentially entered into the tetrahedral Al(2) sites in the spinel block of hexaaluminates. Fe ions in the Al(5) sites of β I-Al 2O 3 and the Al(3) sites of magnetoplumbite phase were highly active for N 2O decomposition.

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