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; Mechanisms of H2O and CO2 Formation from Surface Oxygen Reduction on Co(0001)

机译:; Co(0001)表面氧还原生成H2O和CO2的机理

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Surface O removal by H and CO on Co(0001) has been studied using periodic density functional method (revised Perdew-Burke-Ernzerhof; RPBE) and ab-initio atomistic thermodynamics, On the basis of the quantitative agreement in the H2O formation barrier between experiment (1.34 +/- 0.07 eV) and theory (1.32 eV), H2O formation undergoes a consecutive hydrogenation process [O + 2H -> OH + H -> H2O], while the barrier of H2O formation from OH disproportionation [2OH -> H2O + O] is much lower (0.72 eV). The computed desorption temperatures of H-2 arid H2O under ultrahigh-vacuum conditions agree perfectly with the experiment. Surface O removal by CO has a high barrier (1.41 eV) and is strobsly endothermic (0.94 eV). Precoveted O and OH species do not significantly affect the barriers of H2O and CO2 formation. All of these results indicate that the present RPBE Method and the larger surface Model are more suitable for studying cobalt systems.
机译:使用周期性密度泛函方法(修订版的Perdew-Burke-Ernzerhof; RPBE)和从头算原子热力学研究了H和Co对Co(0001)上表面O的去除,基于H2O形成障碍之间的定量协议根据实验(1.34 +/- 0.07 eV)和理论(1.32 eV),H2O的形成经历了连续的氢化过程[O + 2H-> OH + H-> H2O],而H2O形成的壁垒受到OH歧化的影响[2OH-> H 2 O + O]低得多(0.72 eV)。在超高真空条件下计算出的H-2和H2O的解吸温度与实验完全吻合。通过CO去除表面O的势垒较高(1.41 eV),并且吸热明显(0.94 eV)。令人垂涎的O和OH种类不会显着影响H2O和CO2形成的障碍。所有这些结果表明,目前的RPBE方法和较大的表面模型更适合于研究钴系统。

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