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首页> 外文期刊>The journal of physical chemistry, C. Nanomaterials and interfaces >Unexpected Behavior of Copper in Modified Ferrites during High Temperature WGS Reaction-Aspects of Fe~(3+) - Fe~(2+) Redox Chemistry from Mossbauer and XPS Studies
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Unexpected Behavior of Copper in Modified Ferrites during High Temperature WGS Reaction-Aspects of Fe~(3+) - Fe~(2+) Redox Chemistry from Mossbauer and XPS Studies

机译:高温WGS反应过程中改性铁素体中铜的意外行为-Mossbauer的Fe〜(3+)<-> Fe〜(2+)氧化还原化学和XPS研究

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We report dynamic alternation of the redox chemistry of the Fe~(3+)/ Fe~(2+) 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-M_xO_y-CuO_x 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 hightemperature 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 "5". The Mossbauer spectra and XPS measurements show that Cu plays a different role on Fe~(3+)/Fe~(2+) 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 Fe~(2+) 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.
机译:我们报道了在Cu共掺杂的M-改性铁氧体催化剂中高温水煤气变换反应过程中磁铁矿中Fe〜(3 +)/ Fe〜(2+)对的氧化还原化学反应的动态变化。使用工业经济和环境友好的共沉淀方法合成了M = Cr,Ce,Ni,Co,Mn和Zn的Fe2O3-M_xO_y-CuO_x类型的各种半固态固溶体。有趣的是,在高温WGS反应过程中,Cu在M改性铁氧体中表现出不同寻常的作用。值得注意的是,我们的位移活性测量结果表明,除了M = Ce以外,Cu充当所有M修饰的铁氧体的促进剂,其中M = Cr,Ni,Co,Mn和Zn。对于后一种情况,Cu充当高温WGS反应的抑制剂。程序升温还原测量(TPR)表明,在所有改性铁氧体催化剂中,Cu选择性地促进赤铁矿(Fe2O3)还原为磁铁矿(Fe3O4)。但是,Cu不会促进铁素体中磁铁矿还原为铁素体或其他金属氧化物的还原(预期M = Ce)。 Mossbauer效应研究表明,将Cu共掺杂在磁铁矿中时,Fe局部环境会发生变形。这些畸变反映在八面体(O_h)位置的内部磁场中,其特征异构体位移为“ 5”。 Mossbauer光谱和XPS测量表明,Cu在块体和表面的Fe〜(3 +)/ Fe〜(2+)氧化还原化学中起着不同的作用。在活化过程中,一些铜进入磁铁矿的O_h位置,并取代Fe〜(2+)离子,其余的Cu形成除Fe / Ce外的金属Cu物种。这种双重促进作用负责在铜共掺杂的M改性铁氧体中观察到的高温WGS活性。对于M = Ce,表征研究表明Ce和Cu都在活化后交替进入氧化铁晶格,并与磁铁矿相一起形成了辉石(FeO)相。在Fe / Ce催化剂的Cu共掺杂时,生成铁矿(FeO)导致WGS活性降低。

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