Two different samples of natural zeolite have been investigated by X-band electron paramagnetic resonance (EPR) spectroscopy. The observed EPR spectra are typical to those observed for Fe3+ and Mn2+ ions. The lines, related to the iron, are observed, respectively at g approximate to 4.3 and g approximate to 2. The observed six lines, at g approximate to 2, are the hyperfine structure due to the Mn2+ ions. The simulation of the experimental EPR spectra suggests that both of the manganese and the iron are present in more one site. The temperature dependence of the EPR spectra has been also investigated. The nature of the different sites involved in the EPR absorption is discussed. (C) 2004 Elsevier Ltd. All rights reserved.</p
A natural sample of clinochlore from the Longitudinal Valley area of northeastern Taiwan has been ch...
The number of electron paramagnetic resonance (EPR) parameters for copper(I1) ions held in lattice p...
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Samples of Araucaria area soil from Parana state, Brazil, were separated by particle size fractionat...
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Natural sepiolite minerals and their ?-irradiated forms were investigated by electron paramagnetic r...
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Structural Fe3+ in kaolinites and dickites covering a broad range of disorder was investigated using...
The systematic study of iron-doped MFI zeolite and MFI silicalite by X-and Q-band EPR spectroscopy i...
Natural sepiolite minerals and their gamma-irradiated forms were investigated by electron paramagnet...
Iron(III)-doped zeolites of MFI structure have attracted considerable interest since they are effect...
International audienceStructural Fe 3+ in kaolinites and dickites covering a broad range of disorder...
The method of electron paramagnetic resonance (EPR) was used to identify the characteristics of the ...
The Fe3+ substituted for Al3+ at the 2 octahedral positions is one of the most common impurities in ...
A natural sample of clinochlore from the Longitudinal Valley area of northeastern Taiwan has been ch...
The number of electron paramagnetic resonance (EPR) parameters for copper(I1) ions held in lattice p...
Electron spin resonance (EPR) studies in zeolites are reviewed in which radiolysis was used to ioniz...
Samples of Araucaria area soil from Parana state, Brazil, were separated by particle size fractionat...
Electron paramagnetic resonance (EPR) spectro-scopy is an analytical tool for the identification of ...
nite of different grain size pillared with Zr by interaction with perylene (Pe) and tetracyanoethyle...
Natural sepiolite minerals and their ?-irradiated forms were investigated by electron paramagnetic r...
The adsorption mechanisms of divalent cations in zeolite nanopore channels can vary as a function of...
Structural Fe3+ in kaolinites and dickites covering a broad range of disorder was investigated using...
The systematic study of iron-doped MFI zeolite and MFI silicalite by X-and Q-band EPR spectroscopy i...
Natural sepiolite minerals and their gamma-irradiated forms were investigated by electron paramagnet...
Iron(III)-doped zeolites of MFI structure have attracted considerable interest since they are effect...
International audienceStructural Fe 3+ in kaolinites and dickites covering a broad range of disorder...
The method of electron paramagnetic resonance (EPR) was used to identify the characteristics of the ...
The Fe3+ substituted for Al3+ at the 2 octahedral positions is one of the most common impurities in ...
A natural sample of clinochlore from the Longitudinal Valley area of northeastern Taiwan has been ch...
The number of electron paramagnetic resonance (EPR) parameters for copper(I1) ions held in lattice p...
Electron spin resonance (EPR) studies in zeolites are reviewed in which radiolysis was used to ioniz...