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Received February 13, 2008
Accepted March 29, 2008
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Hydrothermal synthesis and characterization of Fe(III)-substituted mordenites
Department of Advanced Material Chemistry, Shinsung University, Dangjin-gun 343-861, Korea 1Department of Chemical Engineering, Hanseo University, Seosan 356-706, Korea 2Department of Chemical Engineering, College of Engineering, Inha University, Incheon 402-751, Korea
Korean Journal of Chemical Engineering, November 2008, 25(6), 1286-1291(6), 10.1007/s11814-008-0211-2
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Abstract
Fe-substituted mordenites were synthesized hydrothermally, partially substituting iron atoms for the framework aluminum of mordenite. XRD, SEM, IR, UV-VIS DRS, ESR, XAS, and catalytic activity studies provided the evidence of Fe^(3+) present in the zeolite framework. The framework IR bands were shifted to lower frequencies as Fe^(3+) ions incorporated into the lattice, and a new Si-O-Fe bond vibration was located near 668 cm.1. The presence of a signal at g=4.3 in the ESR spectra was assigned to Fe^(3+) isomorphously substituted in the tetrahedral position. EXAFS at the Fe K-edge revealed that the Fe^(3+) ions were present in the zeolite framework in a four-fold coordination with an average Fe-O distance of 1.86 A. In the UV-vis spectra, an absorption was observed at 375.7 nm which was assigned to the presence of Fe^(3+) in the zeolite framework. A toluene alkylation study reflected that the acidity strength of mordenite_x000D_
is weakened due to the presence of lattice iron species.
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