0 having the same kind of magnetism (= power to attract other objects) that iron has
1 having the same kind of magnetism (= power to attract other objects) that iron has
Convective instability of a ferromagnetic fluid is predicted for a fluid layer heated from below in the presence of a uniform vertical magnetic field.
Relevant examples are given by continuum limits of ferromagnetic king systems in equilibrium statistical mechanics.
The nonlinearity in the magnetic system is due to the dependence of the permeability on the induction in ferromagnetic materials.
However, they present an efficient algorithm for the ferromagnetic case, which approximates the partition function, provided that the system is consistent.
However, there are no ferromagnetic cores in the transformers; magnetic saturation will not be formed in the case of intense current flowing primary winding.
Ferromagnetic couplings tend to align the spins, antiferromagnetic couplings make them point in opposite directions.
We mention that (2.23) must not consider the jump of the magnetic permeability at the interface of the ferromagnetic material.
A new model for the study of ferromagnetic thin films is presented.
