Orientation effects in soft X-ray magnetic circular dichroism
Autor: | J. van Elp, B.G Searle |
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Rok vydání: | 1997 |
Předmět: |
Radiation
Absorption spectroscopy Condensed matter physics Chemistry Magnetic circular dichroism Condensed Matter Physics Polarization (waves) Atomic and Molecular Physics and Optics Electronic Optical and Magnetic Materials Magnetic field Paramagnetism X-ray magnetic circular dichroism Local symmetry Physical and Theoretical Chemistry Multiplet Spectroscopy |
Zdroj: | Journal of Electron Spectroscopy and Related Phenomena. 86:93-106 |
ISSN: | 0368-2048 |
DOI: | 10.1016/s0368-2048(97)00051-0 |
Popis: | The orientation dependence of magnetic circular dichroism (MCD) at soft X-ray absorption edges is discussed for paramagnetic 3d transition metal systems using ligand-field atomic multiplet calculations. Previous calculations have used a magnetic orientation along the z axis of the transition metal site. In the present work, three orientation directions are calculated: [001], [110] and [111]. Also an at-random spectrum is calculated which represents the actual situation for 3d transition metals in metalloproteins. The systems investigated can be divided into three classes based on the difference between the MCD effect for the different orientations. The first class contains spherical systems like, for instance, Fe 3+ (d 5 ) systems in O h and T d symmetries and Ni 2+ in O h symmetry. The differences between different orientations in these systems are small, or even absent. The second class contains first-class systems with a distorted local symmetry like Fe 3+ in D 2d symmetry and Ni 2+ in D 4h symmetry. The differences between the different orientations can be quite strong and result from differences in polarization for the left and right circularly polarized absorption spectra. The third-class systems exhibit relatively large zero-field splittings. The differences are very strong and are a result of the interaction between the zero-field splittings and the applied magnetic field. An example is Fe 2+ in D 2d symmetry. |
Databáze: | OpenAIRE |
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