- Source: 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
Verwey transition – Low-temperature phase transition in magnetite
Ferromagnetism – Mechanism by which materials form into and are attracted to magnets
Antiferromagnetism – Regular pattern of magnetic moment ordering
Paramagnetism – Weak, attractive magnetism possessed by most elements and some compounds
Néel temperature – Temperature above which magnetic properties changePages displaying short descriptions of redirect targets
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.
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