Morin transition
The Morin transition (also known as a spin-flop transition) is a magnetic phase transition in α-Fe2O3 hematite where the antiferromagnetic ordering is reorganized from being aligned perpendicular to the c-axis to be aligned parallel to the c-axis below TM.
TM = 260K for Fe3+ in α-Fe2O3.
A change in magnetic properties takes place at the Morin transition temperature.
See also[]
References[]
- Woods, G. T.; Callcott, T. A. (2000). "X-ray magnetic linear dichroism in α-Fe2O3". APS March Meeting Abstracts. Bibcode:2000APS..MARA24005W. Retrieved 2022-01-21.
Categories:
- Magnetic ordering
- Phase transitions