4.6 Article

Unexpected Behavior of Copper in Modified Ferrites during High Temperature WGS Reaction-Aspects of Fe3+ ⇆ Fe2+ Redox Chemistry from Mossbauer and XPS Studies

期刊

JOURNAL OF PHYSICAL CHEMISTRY C
卷 116, 期 20, 页码 11019-11031

出版社

AMER CHEMICAL SOC
DOI: 10.1021/jp301090d

关键词

-

资金

  1. U.S. Department of Energy [DE-PS36-03GO93007]
  2. Ohio Air Quality Development Authority [AY08-09-C21]

向作者/读者索取更多资源

We report dynamic alternation of the redox chemistry of the Fe3+/Fe2+ couple in magnetite during high temperature water-gas shift reaction in Cu codoped M-modified ferrite catalysts. Various hematitic solid solutions of the type Fe2O3-MxOy-CuOx with M = Cr, Ce, Ni, Co, Mn, and Zn are synthesized using the industrially economical and environmentally friendly coprecipitation method. Interestingly, Cu shows an unusual effect in the M-modified ferrites during the high temperature WGS reaction. Remarkably, our shift activity measurements reveal that Cu act as a promoter for all M-modified ferrites with M = Cr, Ni, Co, Mn, and Zn except M = Ce. For the latter case, Cu acts as an inhibitor for the high temperature WGS reaction. Temperature programmed reduction measurements (TPR) show that Cu selectively promotes the reduction of hematite (Fe2O3) to magnetite (Fe3O4) in all modified ferrite catalysts. However, Cu does not promote the reduction of magnetite to wustite or reduction of other metal oxide present in the ferrite expect for M = Ce. Mossbauer effect studies show distortions in the Fe local environments when Cu is codoped in magnetite. These distortions are reflected in the internal magnetic field at octahedral (O-h) sites with characteristic isomer shift delta. The Mossbauer spectra and XPS measurements show that Cu plays a different role on Fe3+/Fe2+ redox chemistry in the bulk and surface. During the activation, some of the Cu enters at the O-h sites of the magnetite and replaces Fe2+ ions and the remaining Cu forms metallic Cu species except for the Fe/Ce. This dual promotional role is responsible for the observed high temperature WGS activity in Cu codoped M-modified ferrites. For M = Ce, characterization studies show that both Ce and Cu enter the iron oxide lattice substitutionally upon activation and form the wustite (FeO) phase along with the magnetite phase. The formation of wustite (FeO) is responsible for the decreased WGS activity upon Cu codoping of Fe/Ce catalyst.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.6
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据