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Influence of the support on rhodium speciation and catalytic activity of rhodium-based catalysts for total oxidation of methane

催化作用 甲烷 化学 遗传算法 有机化学 生物 进化生物学
作者
Yu Zhang,Peter Glarborg,Martin Andersson,Keld Johansen,Thomas Klint Torp,Anker Degn Jensen,Jakob Munkholt Christensen
出处
期刊:Catalysis Science & Technology [Royal Society of Chemistry]
卷期号:10 (17): 6035-6044 被引量:11
标识
DOI:10.1039/d0cy00847h
摘要

The role of the support in Rh-based catalysts for total oxidation of CH4was investigated using both amorphous SiO2and γ-Al2O3as well as ZSM-5 and SSZ-13 zeolites with varying SiO2/Al2O3ratios. The methane oxidation activity was measured in both the presence and absence of 5 vol% H2O and 20 ppm SO2. The support had a strong impact on Rh speciation (Rh2O3nanoparticlesvs.single Rh atom sites), which was important for the activity, as the nanoparticle sites were found to be far more active than the single atom sites. A 2 wt% Rh/ZSM-5(SiO2/Al2O3= 280) catalyst with Rh exclusively as Rh2O3nanoparticles was able to provide oxidation at a 75 °C lower temperature than an ion-exchanged 0.294 wt% Rh/ZSM-5(SiO2/Al2O3= 30) catalyst with Rh exclusively as single atoms despite a similar concentration of active sites in the two samples. All the catalysts were inhibited by the presence of water, but this inhibition was particularly strong for an amorphous SiO2support and for the most Al-rich zeolites and less severe for Si-rich zeolites. The inhibition from SO2was relatively stronger for the more Al-rich supports, which was attributed to an uptake of sulfur at Al sites that was detrimental to the performance of the active phase. In a realistic gas atmosphere containing both H2O and SO2, Si-rich ZSM-5(SiO2/Al2O3= 280) therefore emerged as the best support. This was because the low acidity ensured minimal loss of Rh to the less active single atom sites, avoidance of the detrimental sulfur uptake by the support seen for more Al-rich supports, and avoidance of the strong water-induced inhibition that occurs for amorphous SiO2and Al-rich zeolites.
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