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Intrinsic Catalytic Role of Mesoporous Silica in Preferential Oxidation of Carbon Monoxide in Excess Hydrogen
Author(s) -
Huang Shengjun,
Hara Kenji,
Fukuoka Atsushi
Publication year - 2012
Publication title -
chemistry – a european journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.687
H-Index - 242
eISSN - 1521-3765
pISSN - 0947-6539
DOI - 10.1002/chem.201102256
Subject(s) - catalysis , calcination , mcm 41 , carbon monoxide , mesoporous silica , mesoporous material , prox , chemistry , heterogeneous catalysis , chemical engineering , hydrogen , inorganic chemistry , materials science , organic chemistry , engineering
We have studied the intrinsic catalytic role of MCM‐41 mesoporous silica in preferential oxidation of CO in excess H 2 (PROX). Two types of MCM‐41 supports (MCM‐41A and MCM‐41B) were obtained from the same pristine as‐synthesized materials by using different procedures for surfactant removal: one‐step calcination or two‐step extraction–calcination. Although two kinds of Pt catalysts prepared from the MCM‐41 supports exhibit high similarity in apparent physicochemical parameters such as Pt morphology, particle‐size distribution, electronic states, support architecture, and pore‐size distribution, they show a dramatic difference in catalytic activity (ca. 100 % versus 10 % CO conversions at 298 K). This feature motivated us to investigate the catalytic role of MCM‐41 in the PROX reaction. By means of infrared experiments with the isotope tracer technique, it was revealed that the reactive microenvironment at the interface between Pt and the MCM‐41A support is the origin of the high activity. On the highly active Pt/MCM‐41A catalyst, interfacial silanols play a decisive role in the ignition of CO oxidation, and gaseous O 2 and H 2 are dissociated on CO‐free Pt sites created by the interfacial reaction. The dissociated oxygen and hydrogen are proposed to sustain the catalytic cycle in the form of regenerated silanols on the support, which is catalyzed by the Pt surface in the presence of H 2 .