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  Interplay of Fe and Tm moments through the spin-reorientation transition in TmFe O3

Staub, U., Rettig, L., Bothschafter, E. M., Windsor, Y. W., Ramakrishnan, M., Avula, S. R. V., et al. (2017). Interplay of Fe and Tm moments through the spin-reorientation transition in TmFe O3. Physical Review B, 96(17): 174408. doi:10.1103/PhysRevB.96.174408.

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PhysRevB.96.174408.pdf (Verlagsversion), 3MB
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PhysRevB.96.174408.pdf
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2017
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APS
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 Urheber:
Staub, U.1, Autor
Rettig, Laurenz1, 2, Autor           
Bothschafter, E. M.1, Autor
Windsor, Yaov William1, 2, Autor           
Ramakrishnan, M.1, Autor
Avula, S. R. V.1, Autor
Dreiser, J.1, Autor
Piamonteze, C.1, Autor
Scagnoli, V.3, 4, Autor
Mukherjee, S.5, Autor
Niedermayer, C.5, Autor
Medarde, M.4, Autor
Pomjakushina, E.4, Autor
Affiliations:
1Swiss Light Source, Paul Scherrer Institut, CH-5232 Villigen PSI, Switzerland, ou_persistent22              
2Physical Chemistry, Fritz Haber Institute, Max Planck Society, ou_634546              
3Laboratory for Mesoscopic Systems, Department of Materials, ETH Zurich, 8093 Zurich, Switzerland, ou_persistent22              
4Laboratory for Multiscale Materials Experiments, Paul Scherrer Institut, 5232 Villigen PSI, Switzerland, ou_persistent22              
5Laboratory for Neutron Scattering and Imaging, Paul Scherrer Institut, 5232 Villigen PSI, Switzerland, ou_persistent22              

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 Zusammenfassung: X-ray magnetic circular dichroism (XMCD) and x-ray magnetic linear dichroism (XMLD) have been used to investigate the Fe magnetic response during the spin-reorientation transition (SRT) in TmFeO3. Comparing the Fe XMLD results with neutron-diffraction and magnetization measurements on the same sample indicates that the SRT has an enhanced temperature range in the near surface region of approximately 82 to 120 K compared to approximately 82 to 92 K in bulk. This view is supported by complementary resonant soft x-ray- diffraction experiments at the Tm M5 edge. These measurements find an induced magnetic moment on the Tm sites, which is well described by a dipolar mean-field model originating from the Fe moments. Even though such a model can describe the 4ƒ response in the experiments, it is insufficient to describe the SRT even when considering a change in the 4ƒ anisotropy. Moreover, the results of the Fe XMCD show a different temperature evolution through the SRT, the interpretation of which is hampered by additional spectral shape changes of the XCMD signal.

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Sprache(n): eng - English
 Datum: 2017-08-022017-05-262017-11-072017-11-01
 Publikationsstatus: Erschienen
 Seiten: 11
 Ort, Verlag, Ausgabe: -
 Inhaltsverzeichnis: -
 Art der Begutachtung: Expertenbegutachtung
 Identifikatoren: DOI: 10.1103/PhysRevB.96.174408
 Art des Abschluß: -

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Projektname : International Fellowship Program on PSI-FELLOW - Materials & Matter, Energy & Environment, Human Health & Life-Sciences, and Accelerator Technology
Grant ID : 290605
Förderprogramm : Funding Programme 7 (FP7)
Förderorganisation : European Commission (EC)

Quelle 1

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Titel: Physical Review B
  Kurztitel : Phys. Rev. B
Genre der Quelle: Zeitschrift
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Affiliations:
Ort, Verlag, Ausgabe: Woodbury, NY : American Physical Society
Seiten: 11 Band / Heft: 96 (17) Artikelnummer: 174408 Start- / Endseite: - Identifikator: ISSN: 1098-0121
CoNE: https://pure.mpg.de/cone/journals/resource/954925225008