Jump to content

Morin transition

From Wikipedia, the free encyclopedia
This is an old revision of this page, as edited by 65.10.252.225 (talk) at 23:42, 7 February 2010. The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

The Morin 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


Retrieved from "https://en.wikipedia.org/w/index.php?title=Morin_transition&oldid=342585863"