Catalytic reduction of NO with H sub(2) over redox-cycling Fe on CeO sub(2)

Removal of NO sub(x) species from automotive emissions continues to be a challenge, particularly using replacements for Pt-group metals. Here, we demonstrate the synthesis of FeO sub(x) domains on CeO sub(2) from the precursor Fe ethylenediaminetetraacetate (NaFeEDTA) and its utility in the reductio...

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Veröffentlicht in:Applied catalysis. B, Environmental Environmental, 2015-06, Vol.168-169, p.68-76
Hauptverfasser: Prieto-Centurion, Dario, Eaton, Todd R, Roberts, Charles A, Fanson, Paul T, Notestein, Justin M
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Sprache:eng
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Zusammenfassung:Removal of NO sub(x) species from automotive emissions continues to be a challenge, particularly using replacements for Pt-group metals. Here, we demonstrate the synthesis of FeO sub(x) domains on CeO sub(2) from the precursor Fe ethylenediaminetetraacetate (NaFeEDTA) and its utility in the reduction of NO with H sub(2) as a model reaction for tailpipe emissions. Diffuse-reflectance UV-visible and X-ray absorption near-edge spectroscopies indicate the formation of small, non-crystalline FeO sub(x) domains. Using the EDTA precursor, TPR and in situ XANES show that up to 45% of the FeO sub(x) centers were capable of undergoing redox cycles in H sub(2) up to 550 [degrees]C, whereas only 23% of FeO sub(x) centers derived from Fe(NO sub(3)) sub(3) were redox active. Similarly, at comparable Fe surface densities, the FeEDTA-derived catalysts were more active than the nitrate-derived materials in the reduction of NO to N sub(2) (85-95% selectivity) with H sub(2) at 450 [degrees]C. The presence of both the bulky organic ligand and the alkali is essential for the observed enhancements in fraction redox active and to achieve high NO reduction rates. Rates over all materials were fit to a single correlation against the number of redox-active FeO sub(x) centers, suggesting that these are the catalytic active sites. The new materials describe here may offer new avenues for emissions control without Pt-group metals or substituted zeolites.
ISSN:0926-3373
DOI:10.1016/j.apcatb.2014.11.055