2004
DOI: 10.1016/j.jcat.2004.03.032
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Mechanism and kinetics of the selective NO reduction over Co-ZSM-5 studied by the SSITKA technique

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Cited by 46 publications
(14 citation statements)
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“…With further increasing the cobalt loading ratio, excess cobalt coexisting in small Co x O y clusters (CoO, Co 2 O 3 , Co 3 O 4 , etc.) constitute the majority of the species in overexchanged catalysts , and are potentially a good candidate for performing SCR activity at the HT-peak (Figure ), resulting in the HT-peak shifting toward lower temperatures. With increasing cobalt content, the P NO at the HT-peak shows a declining trend after an initial ascent.…”
Section: Resultsmentioning
confidence: 99%
“…With further increasing the cobalt loading ratio, excess cobalt coexisting in small Co x O y clusters (CoO, Co 2 O 3 , Co 3 O 4 , etc.) constitute the majority of the species in overexchanged catalysts , and are potentially a good candidate for performing SCR activity at the HT-peak (Figure ), resulting in the HT-peak shifting toward lower temperatures. With increasing cobalt content, the P NO at the HT-peak shows a declining trend after an initial ascent.…”
Section: Resultsmentioning
confidence: 99%
“…Cobalt zeolites are important catalysts for the selective catalytic reduction (SCR) of nitrogen oxides by hydrocarbons, especially by methane [1][2][3][4][5][6][7][8][9][10][11][12][13][14]. It is widely accepted that depending on the used zeolite, its Si/Al ratio, Co content, and preparation method, different Co species are formed comprising: (i) Co 2+ cations located in the zeolite channels, (ii) CoO x microaggregates, and (iii) CoO, Co 3 O 4 , as well as Co silicate mainly in the case of over-exchanged zeolites.…”
Section: Introductionmentioning
confidence: 99%
“…In the oxidized form cobalt-containing zeolites, such as Co-FER, Co-MFI and Co-MOR, are active catalysts for reducing NO with methane in oxidizing atmosphere, so allowing the denitrification (DeNOxing) of waste gases. Co 2+ ions exchanging the protons of the protonic zeolites are considered to be the active sites in the reaction, while other authors suggested the presence of “extraframework” CoOx oxide clusters to represent the catalytically active species . In a series of recent papers the UV–vis spectra of Co-FER, Co-MFI and Co-MOR have been studied in detail and assigned to Co 2+ ions in different locations in the zeolite cavities. The possible cooperation of residual protonic sites and Co cationic sites in partially exchanged Co-zeolites for the CH 4 –SCR reaction has also been discussed .…”
Section: Introductionmentioning
confidence: 99%