AVS 61st International Symposium & Exhibition | |
In-Situ Spectroscopy and Microscopy Focus Topic | Tuesday Sessions |
Session IS+AS+MC+SS-TuM |
Session: | Ambient Pressure X-ray Photoelectron Spectroscopy (AP-XPS) |
Presenter: | Weixin Huang, University of Notre Dame |
Authors: | F. Tao, University of Notre Dame J. Shan, University of Notre Dame L.T. Nguyen, University of Notre Dame S. Zhang, University of Notre Dame W. Huang, University of Notre Dame |
Correspondent: | Click to Email |
It is critical to develop a catalyst made of earth-abundant elements highly active for a complete combustion of CH4 at a relatively low temperature for catalytically transforming CH4 to electrical energy in power plant. The currently available catalysts with high activity consist of precious metal nanoparticles supported on rare earth oxides. Their high cost limits the application of these catalysts at industrial scale. Here we report a new catalyst, early transition metal oxide-based mixed oxide only consisting of earth-abundant elements which can completely combust CH4 at 350oC at a gas hourly space velocity of 240,000 ml 0.5% CH4 on 1 gram in one hour. This comparable or even higher catalytic activity results from the integration of Ni cations and surface lattice oxygen atoms at the atomic scale. With such an integration, the carbon atom dissociated from CH4 can bond with its neighboring surface oxygen atoms to form an intermediate of CO2 and then desorb.
In-situ studies of catalyst surface using AP-XPS and monitoring of products formed from isotope-labeled catalysts show that (1) molecules O2 dissociates on surface oxygen vacancies, (2) half of the dissociated oxygen atoms stay in oxygen vacancies, (3) the other half of dissociated oxygen atoms directly bond with hydrogen atoms dissociated from CH4 to from OH and then H2O molecules, (4) CH4 progressively dissociates on Ni cations to form CHn (n=3, 2, 1, 0), (5) carbon atoms bind to two surface lattice oxygen atoms nearby to form a carboxylate species, O-C-O intermediate, and then desorb. The mixed cations and surface lattice oxygen atoms in this mixed oxide at atomic level makes the formation of an –O-C-O- intermediate at a mild temperature since a spillover of dissociated species is not necessary.