Abstract
Rare-earth-based permanent-magnet materials rich in iron have relatively low ferromagnetic ordering temperatures. This is believed to be due to the presence of antiferromagnetic exchange interactions, besides the ferromagnetic interactions responsible for the magnetic order. The magnetic properties of are anomalous. Instead of ferromagnetic, it is antiferromagnetic, and instead of one ordering temperature, it shows two, at the Néel temperature and at . , doped by 0.5% Ta, also shows two ordering temperatures, one to an antiferromagnetic phase, at , and one to a ferromagnetic phase, at . In order to clarify this behavior, single-crystalline samples were prepared by solution growth and characterized by electron microscopy, single-crystal x-ray diffraction, temperature-dependent specific heat, and magnetic field and temperature-dependent electrical resistivity and magnetization. From these measurements, magnetic phase diagrams were determined for both Ta-doped and undoped . These phase diagrams can be very well described in terms of a theory that gives magnetic phase diagrams of systems with competing antiferro- and ferromagnetism.
9 More- Received 22 December 2006
DOI:https://doi.org/10.1103/PhysRevB.76.054420
©2007 American Physical Society