Importance of the lifetime of oxygen species generated by N2O decomposition for hydrocarbon activation over Fe-silicalite

被引:30
作者
Kondratenko, EV
Pérez-Ramírez, J
机构
[1] Inst Appl Chem, D-12489 Berlin, Germany
[2] ICREA, E-08010 Barcelona, Spain
[3] Inst Chem Res Catalonia ICIQ, Lab Heterogeneous Catalysis, E-43007 Tarragona, Spain
关键词
N2O decomposition; N2O reduction; iron silicalite; oxygen species; C3H8; CH4; mechanism; TAP reactor;
D O I
10.1016/j.apcatb.2005.10.019
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
Transient isotopic studies in the Temporal Analysis of Products (TAP) reactor evidenced a clear mechanistic regularity between methane and propane for N2O reduction over Fe-silicalite in the temperature range of 623-773 K. The lifetime of the oxygen species generated by N2O decomposition on extraframework iron sites was found to be crucial for alkane oxidation. When N2O and CH4 or C3H8 were Pulsed together over Fe-silicalite, oxygen species deposited on iron sites effectively activated the hydrocarbon. However, these oxygen species become inactive for alkane oxidation if the pulses of N2O and the alkane were separated by more than 0.1 s. Transient studies have indicated that C3H8 is more efficient for N2O reduction than CH4, as expected from the facilitated activation of the C-H bond upon increasing the carbon number in alkanes. The performance derived from the TAP reactor agrees well with experiments under flow conditions at ambient pressure. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:35 / 41
页数:7
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