Abstract
The isothermal curves of magnetite in the principal crystallographic directions have been measured from room temperature to the Curie point. These curves give the anisotropy energy and spontaneous magnetization as a function of temperature. Near the Curie point the magnetizing field required to create a single domain is found to be <100 amp/m, giving an unambiguous experimental determination of the spontaneous magnetization in this critical region. Temperature increments of 0.1°C define the Curie point with an uncertainty of <0.05°C. In the neighborhood of the Curie point the curves are very nonlinear; replotting the data in the form of curves at constant magnetization shows that in this region the magnetic energy can be expressed as , where is a constant.
- Received 20 January 1956
DOI:https://doi.org/10.1103/PhysRev.102.959
©1956 American Physical Society