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首页> 外文期刊>ACS Omega >Mn-Doped Maghemite (γ-Fe2O3) from Metal–Organic Framework Accompanying Redox Reaction in a Bimetallic System: The Structural Phase Transitions and Catalytic Activity toward NOx Removal
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Mn-Doped Maghemite (γ-Fe2O3) from Metal–Organic Framework Accompanying Redox Reaction in a Bimetallic System: The Structural Phase Transitions and Catalytic Activity toward NOx Removal

机译:双金属体系中伴随氧化还原反应的金属-有机骨架中掺杂锰的磁赤铁矿(γ-Fe 2 O 3 ):结构相变和催化活性对NOx的去除

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Mn-doped maghemite (γ-Fe_(2)O_(3)) particles were generated from a binary metal (Fe,Mn)-based metal–organic framework (MOF) via thermal decomposition under air. The X-ray photoelectron spectroscopy analysis revealed that the synthesis of Fe/Mn-MOF accompanied the reduction of the metal ions. The existence of Mn ions in this synthetic process leads to thermally stable maghemite particles under air. A temperature-induced structural phase transition from γ-Fe_(2)O_(3) to α-Fe_(2)O_(3) was observed through a mixed phase with another structure. Mn-doped γ-Fe_(2)O_(3) and α-Fe_(2)O_(3) exhibit superparamagnetic behavior. The sample annealed at 600 °C showed a mixed magnetic hysteresis loop indicating the existence of an intermediate structural phase between γ-Fe_(2)O_(3) and α-Fe_(2)O_(3) during the phase conversion from FeMn-MOF. The constructed Mn-doped iron oxides are active toward reducing nitric oxide with NH_(3). The NO conversion is 97% over Mn-doped γ-Fe_(2)O_(3) calcined at 320 °C.
机译:锰掺杂的磁赤铁矿(γ-Fe_(2)O_(3))颗粒是由二元金属(Fe,Mn)基金属-有机骨架(MOF)在空气中热分解产生的。 X射线光电子能谱分析表明,Fe / Mn-MOF的合成伴随着金属离子的还原。在这种合成过程中,Mn离子的存在导致在空气中热稳定的磁赤铁矿颗粒。通过与另一种结构的混合相观察到温度诱导的结构相从γ-Fe_(2)O_(3)转变为α-Fe_(2)O_(3)。 Mn掺杂的γ-Fe_(2)O_(3)和α-Fe_(2)O_(3)表现出超顺磁行为。在600°C退火的样品表现出混合磁滞回线,表明在从FeMn-的相转化过程中存在γ-Fe_(2)O_(3)和α-Fe_(2)O_(3)之间的中间结构相。 MOF。所构建的Mn掺杂的氧化铁具有用NH_(3)还原一氧化氮的活性。相对于在320°C下煅烧的Mn掺杂γ-Fe_(2)O_(3),NO转化率为97%。

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