Ferrimagnetism has opposing, generally unequal ordered magnetic sublattices, with net magnetization in a collinear model. Louis Néel used it to explain magnetic oxides.[ref]
The counting example in magnetic sublattice gives . Unequal populations also suffice: four sites carrying and two carrying give , even with identical individual magnitudes. Thus one must compare total sublattice contributions per common volume, rather than merely asking whether two atomic species carry different magnetic moments.
Both ferromagnetism and ferrimagnetism can produce a macroscopic magnet. Their internal organization differs: the latter retains opposing contributions. This makes ferrimagnetism a useful bridge between net magnetization and microscopic magnetic order: reducing one opposing contribution can increase the net sum, even though the total sum of moment magnitudes decreases.
At a magnetic compensation temperature, : an ordered ferrimagnet has zero net magnetization. Such cancellation need not occur in every material.[ref]
For an original stipulated example, let , with , and prescribe sublattice magnitudes per common volume by
Take A along and B along , retaining a fixed sublattice orientation convention. These are toy functions, not measured curves or a self-consistent mean-field approximation. Their difference factors exactly:
At , . At , both magnitudes equal and : this is compensation with finite order. At , . At , both magnitudes vanish: that endpoint represents the stipulated Curie temperature, not another compensation point. For stipulate both ordered magnitudes zero; do not extrapolate the polynomials into negative sublattice magnitudes.
The sign change refers to the net component relative to the fixed A direction. A freely reorienting specimen in an applied magnetic field need not display this signed branch directly. The example isolates the cancellation mechanism; it predicts neither a material's transition temperature nor its response to magnetic domains or an applied magnetic field.

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Ferrimagnetism is a type of magnetic ordering that occurs in certain materials, where the magnetic moments of atoms or ions align in opposite directions but unequal magnitudes. This results in a net magnetic moment even though the opposing moments partially cancel each other out. In ferrimagnetic materials, typically found in certain types of oxides (like magnetite, Fe3O4), there are two different types of magnetic ions or sublattices with unequal magnetic moments.