Abstract
Charge mismatch at the interface between canted antiferromagnetichematite (alpha-Fe2O3) and antiferromagnetic ilmenite (FeTiO3) isaccommodated by the formation of mixed Fe2+ and Fe3+ contact layers,leading to uncompensated magnetic moments in the system. To derive themagnetic exchange interaction parameters of the end members andinterface, we map total-energy differences of collinear spinarrangements obtained from density-functional theory calculations to aHeisenberg Hamiltonian using the least-squares method. Parameters forthe end members, hematite (J(m)(3+,3+)) and ilmenite (J(m)(2+),(2+)) arein good agreement with the values obtained from inelasticneutron-scattering data. The magnetic interaction parameters betweenFe2+ and Fe3+ (J(m)(2+,3+)) in the contact layer show a strongantiferromagnetic coupling to the adjacent hematite layers and thusexplain the ferrimagnetism in the system.
Dokumententyp: | Zeitschriftenartikel |
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Fakultät: | Geowissenschaften > Department für Geo- und Umweltwissenschaften > Kristallographie und Materialwissenschaft |
Themengebiete: | 500 Naturwissenschaften und Mathematik > 530 Physik
500 Naturwissenschaften und Mathematik > 540 Chemie 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie |
Sprache: | Englisch |
Dokumenten ID: | 18851 |
Datum der Veröffentlichung auf Open Access LMU: | 10. Mrz. 2014, 14:16 |
Letzte Änderungen: | 04. Nov. 2020, 13:00 |