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.
Item Type: | Journal article |
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Faculties: | Geosciences > Department of Earth and Environmental Sciences > Crystallography and Materials Science |
Subjects: | 500 Science > 530 Physics 500 Science > 540 Chemistry 500 Science > 550 Earth sciences and geology |
Language: | English |
Item ID: | 18851 |
Date Deposited: | 10. Mar 2014, 14:16 |
Last Modified: | 04. Nov 2020, 13:00 |