Theoretical and Experimental Assessments of Elementary Steps and Bound Intermediates in Catalytic H2-O2 Reactions on Dispersed Pt Nanoparticles

被引:0
|
作者
Iglesia, Enrique [1 ]
Mansour, Haefa [1 ]
机构
[1] Univ Calif Berkeley, Dept Chem Engn, Berkeley, CA 94720 USA
基金
美国国家科学基金会;
关键词
FISCHER-TROPSCH SYNTHESIS; TOTAL-ENERGY CALCULATIONS; HYDROGEN-OXYGEN REACTION; PLATINUM; OXIDATION; WATER; PEROXIDE; H-2; DECOMPOSITION; SELECTIVITY;
D O I
10.1021/acs.jpcc.2c08826
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Kinetic and isotopic data and H-2 chemisorption uptakes measured under reaction conditions are combined here with theoretical assessments on model catalytic surfaces at relevant hydrogen (H*) coverages to establish the identity and kinetic relevance of elementary steps and bound species in H-2-O-2 reactions on Pt surfaces. Turnover rates are proportional to O2 pressure and decrease and then reach constant values as H-2 pressures increase, leading to apparent first-order rate parameters (r(O2)/P-O2) that reflect reactive collision probabilities of O-2 with surfaces and which depend solely on the H-2 pressure at all temperatures (540-680 K). H-2-D-2 isotopic exchange rates during reactions with O-2 are much faster than water formation rates, consistent with quasiequilibrated H-2 dissociation steps and with prevalent H* coverages that can be determined independently from H-2 uptakes; such measurements enable the decoupling of non-Langmuirian adsorption parameters from kinetic parameters in rate equations. These data indicate that H-2-O-2 reactions involve two kinetically-relevant O2 dissociation routes. One channel forms two bound O atoms on bare Pt atom ensembles available within H* adlayers, which react via fast subsequent reactions with H* to form H2O. A parallel O-2 dissociation route involves reactions with a H*-H* pair to form weakly bound adsorbed hydrogen peroxide (*HOOH*), a highly reactive species that subsequently cleaves its O-O bond in steps that are not kinetically-relevant. The free-energy barriers are dominated by losses in translational entropy incurred upon the formation of the transition states from their gaseous O-2 precursors. Kinetic isotope effects are near unity for both routes because H* is not involved in direct O-2 dissociation steps, and the *HOOH* formation transition state occurs very early along the reaction coordinate (with nearly intact O-O and Pt-H bonds from reactant states), as confirmed by DFT-derived energies and isotope effects.
引用
收藏
页码:4553 / 4569
页数:17
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