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Pressure-Induced Magnetic Transition in Fe<sub>4</sub>N Probed by Fe<i>K</i>-edge XMCD Measurement
34
Citations
19
References
2003
Year
Magnetic PropertiesX-ray SpectroscopyPressure-induced Magnetic TransitionEngineeringFe Magnetic StatesMagnetic ResonanceMagnetic MaterialsMagnetoresistanceXmcd IntensityMagnetismQuantum MaterialsMaterials SciencePhysicsMagnetic MeasurementMagnetoelasticityMagnetic MaterialFe 4FerromagnetismNatural SciencesX-ray DiffractionApplied PhysicsCondensed Matter PhysicsMagnetic Property
X-ray magnetic circular dichroism (XMCD) of γ'-iron nitride (Fe 4 N) was recorded at Fe K -edge under high pressue up to 27 GPa. The XMCD intensity decreased remarkably with pressure, and vanished at 24 GPa. Compressibility was measured by the X-ray diffraction method. These results indicate that Fe 4 N undergoes a second-order phase transition from the ferromagnetic state to a paramagnetic state without any structural change. The pressure-induced demagnetizing process is discussed in terms of the Fe magnetic states in the local environment.
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