Zobrazeno 1 - 10
of 38
pro vyhledávání: '"J. M. Gaite"'
Publikováno v:
Applied Magnetic Resonance. 21:39-48
An electron paramagnetic resonance (EPR) study of Fe3+ centers in kyanite AlSi2O5 has been performed on a natural blue single crystal at 34.40 GHz. Three Fe3+ centers have been observed. One of them, arising from 10% of the Fe3+ amount, presents weak
Autor:
J. M. Gaite, G. R. Bulka, N. M. Nizamutdinov, A. A. Galeev, V. M. Vinokurov, V. V. Izotov, N. M. Khasanova
Publikováno v:
Journal of Physics: Condensed Matter. 10:7609-7618
A single crystal of doped with was studied by EPR at room temperature and at using an X-band spectrometer. There are two magnetically equivalent spectra characterized by the main Stevens constants and . The spectra are described by a general spin Ham
Autor:
J.-M. Gaite, H. Rager
Publikováno v:
Journal of Physics: Condensed Matter. 9:10033-10039
In an electron paramagnetic resonance study of a synthetic single crystal of forsterite, , one spectrum of with maximum local symmetry -1 was observed. This spectrum arises from substituted for at the position. The second-order constants of the spect
Publikováno v:
Clays and Clay Minerals. 45:496-505
The Fe3+ substituted for Al3+ at the 2 octahedral positions is one of the most common impurities in the kaolinite structure detected by electron paramagnetic resonance (EPR). Evidence has been provided for a relationship between the shape of EPR spec
Publikováno v:
Journal of Physics: Condensed Matter. 3:7877-7886
An EPR study of Fe3+ centres in single crystals of KTiOPO4 (KTP) has been performed. Two crystals grown under identical conditions have been used in the experiment carried out at the Q-band frequency: the first was iron doped and the other was undope
Publikováno v:
Physics and Chemistry of Minerals
Physics and Chemistry of Minerals, Springer Verlag, 2003, 30, pp.(6) 366-372. ⟨10.1007/s00269-003-0325-3⟩
Physics and Chemistry of Minerals, Springer Verlag, 2003, 30, pp.(6) 366-372. ⟨10.1007/s00269-003-0325-3⟩
Only one part of the EPR lines of a kaolinite spectrum of structural Fe 3+ is clearly observable because of the overlapping of other lines with other spectra. For this reason, to determine the structural Fe 3+ concentration we used the line near g=9,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::828ee59bd43c43b65b94f201bea42826
https://hal-insu.archives-ouvertes.fr/hal-00069459
https://hal-insu.archives-ouvertes.fr/hal-00069459
Autor:
J. M. Gaite, Czesław Rudowicz, N. M. Nizamutdinov, V. M. Vinokurov, N. M. Khasanova, G. R. Bulka, A. A. Galeev
Publikováno v:
Journal of Magnetic Resonance
Journal of Magnetic Resonance, Elsevier, 2002, 155, pp.(1) 57-63. ⟨10.1006/jmre.2002.2512⟩
Journal of Magnetic Resonance, Elsevier, 2002, 155, pp.(1) 57-63. ⟨10.1006/jmre.2002.2512⟩
Electron paramagnetic resonance study of a natural single crystal of natrolite was carried out at the frequency nu=36.772 GHz at room temperature. The angular dependence of the four symmetry-related spectra of Fe(3+) in the three crystallographic pla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ae65819a3edeeb81bb8bfae7c589f92f
https://hal-insu.archives-ouvertes.fr/hal-00076878
https://hal-insu.archives-ouvertes.fr/hal-00076878
Publikováno v:
Applied Magnetic Resonance
Applied Magnetic Resonance, Springer Verlag, 2001, 20, pp.307-315. ⟨10.1007/BF03162283⟩
Applied Magnetic Resonance, Springer Verlag, 2001, 20, pp.307-315. ⟨10.1007/BF03162283⟩
Two synthetic beryls (Al2Be3Si6O18) of different color (purple and blue-green) were studied with electron paramagnetic resonance (EPR) and optical spectroscopy. In both crystals, the known spectra of Cu2+ and Fe3+ were observed with the same relative
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dbee4fc66d3721c131d863f48cabe660
https://hal-insu.archives-ouvertes.fr/hal-00089733
https://hal-insu.archives-ouvertes.fr/hal-00089733
Publikováno v:
Physics and Chemistry of Minerals. 20
The electron paramagnetic resonance (EPR) spectra of Fe3+ in a well cristallized kaolinite from Decazeville in France are well resolved. It is shown that in this sample there are mainly two slightly different spectra, well separated at low temperatur
Publikováno v:
Acta Crystallographica Section A Foundations of Crystallography. 56:s365-s365