2020
DOI: 10.1016/j.apsusc.2019.144201
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Diatomite-supported birnessite–type MnO2 catalytic oxidation of formaldehyde: Preparation, performance and mechanism

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Cited by 68 publications
(18 citation statements)
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“…At the same time, two new weak peaks at 569 cm −1 and 641 cm −1 appear which correspond to δ-MnO 2 in PCS-MnO 2 -2. This is consistent with the XRD result [ 38 ].…”
Section: Resultssupporting
confidence: 93%
“…At the same time, two new weak peaks at 569 cm −1 and 641 cm −1 appear which correspond to δ-MnO 2 in PCS-MnO 2 -2. This is consistent with the XRD result [ 38 ].…”
Section: Resultssupporting
confidence: 93%
“…The third stage, at 400–500 °C, was assigned to the removal of the structural hydroxyl. 31 Weight loss at temperatures of 500–800 °C corresponded to the thermal decomposition of MnO 2 , which occurs when temperatures increase, as ascertained via eqn (6) (ref. 32 and 33 ) as follows: …”
Section: Resultsmentioning
confidence: 99%
“…The large amount of Fe 3+ requires the generation of free electron in the crystal Three kinds of surface oxygen species were clearly observed from the O1s spectra in Figure 3c. The one peak located at ~530.1 eV was is assigned to the lattice oxygen species (O latt ), and the peaks located at around 531.6 eV and 532.5 eV are ascribed to the surface adsorbed oxygen (O ads ) and surface hydroxyl oxygen (O OH ) species [22,37], respectively. Literature demonstrates that the surface adsorbed oxygen species play an important role in the deep oxidation of VOCs [12,38].…”
Section: Xps Analysismentioning
confidence: 99%
“…Supports not only improve the distribution of active ingredients, but also contribute to the enhancement of the activity through the interaction with the active species. Recently, the application of natural clay minerals (e.g., palygorskite, diatomite, montmorillonite, and halloysite) for catalytic supports have attracted great attention due to their excellent thermal stability, chemical stability, and abundant mesopores structure [21][22][23]. Palygorskite (Pal) is a natural rod-like clay mineral with the chemical formula of Mg 5 Si 8 O 20 (OH) 2 (H 2 O) 4 •4H 2 O, and aluminum or iron has an obvious substitution of magnesium.…”
Section: Introductionmentioning
confidence: 99%