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Magnetic Collapse in Fe3Se4 under High Pressure
Lyudmila V Begunovich1,2, Maxim M Korshunov1,2, Sergey G Ovchinnikov1,2
1Kirensky Institute of Physics, Federal Research Center KSC SB RAS, Akademgorodok 50/38, 660036 Krasnoyarsk, Russia.
The study reveals that applying pressure to iron selenide (Fe3Se4) alters its magnetic properties, transitioning it from ferrimagnetic to ferromagnetic and eventually to a paramagnetic state. These magnetic changes are linked to electronic structure modifications under compression.
Area of Science:
- Condensed Matter Physics
- Materials Science
- Solid State Chemistry
Background:
- Iron selenide (Fe3Se4) exhibits complex electronic and magnetic properties.
- Understanding its behavior under pressure is crucial for potential applications.
Purpose of the Study:
- To investigate the electronic structure and magnetic properties of Fe3Se4.
- To determine the effects of isotropic compression on its magnetic ordering and total magnetic moment.
Main Methods:
- Density functional theory (DFT) calculations were employed.
- Electronic structure and magnetic moments were computed.
- The impact of varying degrees of isotropic compression was simulated.
Main Results:
- Fe3Se4 is ferrimagnetic with distinct magnetic moments at different iron sites (M1=2.071μB, M2=-2.042μB).
- Compression non-monotonically affects the total magnetic moment and density of states at the Fermi level.
- Magnetic transitions occur: ferrimagnetic to ferromagnetic at 7% compression (5.0 GPa), and to paramagnetic at 14% compression (114 GPa).
- The system remains metallic under all simulated compression levels.
Conclusions:
- Isotropic compression significantly alters the magnetic state of Fe3Se4.
- Anisotropy in chemical bonding accelerates magnetic changes under pressure.
- Fe3Se4 transitions through ferrimagnetic, ferromagnetic, and paramagnetic states with increasing pressure.
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