A material that is magnetic and electrically polarised at the same time, so a magnetic field can shift its charge and an electric field can turn its magnetism. The combination is rare, because the two kinds of order usually want incompatible atoms.
Going deeper
A multiferroic carries magnetic and electric order at once. In the type-II case the two are not merely coexisting: the spin arrangement itself breaks inversion symmetry and produces the polarisation, which is why reversing the spiral reverses the charge.
Two orders that get in each other’s way
The reason multiferroics are rare is chemical. The classic way to make a oxide is to give a transition metal an empty d shell, so it can shift off-centre toward its oxygen neighbours. Magnetism needs the opposite: a partly filled d shell carrying a moment. One ion cannot easily do both.
The workarounds are all indirect. A lone pair of electrons on a heavy ion such as bismuth can drive the displacement while the magnetic ion is left alone, which is how BiFeO3 manages both at room temperature. Geometric distortions, charge ordering, and improper mechanisms where polarisation appears as a by-product of some other structural instability all appear in the catalogue. In each of these type-I cases the two orders have separate causes – and, as a direct consequence, they barely influence one another.
Type II: letting the magnetism do the work
The alternative is to make the responsible for the polarisation. A spiral or cycloidal arrangement can lack a centre of inversion all by itself, and through spin–orbit effects – the inverse or spin-current mechanism – the electrons redistribute slightly, leaving a net electric dipole tied to the of the spiral.
This is what makes type-II multiferroics interesting: the coupling is not an add-on but the origin, so a magnetic field that changes the spiral changes the polarisation, and an electric field can select the handedness. The price is that the polarisation is small, typically a hundred times less than in a conventional ferroelectric, and that it only exists where the spiral does – which is usually well below room temperature.
Down to a single layer
Whether any of this survives in two dimensions is being tested on NiI2. Its nickel layers order into a proper-screw spin helix with a definite handedness, and that handedness couples to the charge to give a polar, chirality-selected state. Circular measurements pick up the magneto-chiral ground state and its electromagnon modes; birefringence and show a state that breaks both three-fold rotation and inversion; and the whole set of signatures follows down to the .
The caveat is that this evidence is optical. Second-harmonic generation and birefringence establish symmetry and a polar state; they are not a measurement of a switchable polarisation with electrodes, which in a single layer of an iodide is a hard experiment. A 2023 reply argued that these optical signatures alone do not establish a single-layer multiferroic. , and stacking in few-layer samples also shift the transition, so the layer-number dependence is part of the physics rather than a detail.
For specialists
A material carrying more than one ferroic order – usually ferroelectric together with (anti)ferromagnetic – plus magnetoelectric coupling between them. Type-I multiferroics have independent origins and weak coupling; in type-II the polarisation is produced by the magnetic order itself, typically a spiral, and the coupling is strong. NiI2 has been reported to keep a type-II order, with spiral magnetism and polarisation appearing together, down to the single layer – although the optical evidence is disputed.