A phenomenon where a magnetic field induces transverse heat flow in materials.The anomalous Hall effect is a phenomenon where an electric current flowing through a magnetic material produces a transverse voltage—perpendicular to both the current and the magnetization—without requiring an external magnetic field. Unlike the ordinary Hall effect, which arises from the Lorentz force on moving charges, the anomalous version originates from the material's internal magnetization and relativistic spin–orbit coupling. This effect is a cornerstone of spintronics and provides a probe of the quantum geometry of electronic wavefunctions in solids.
The effect was discovered by Edwin Hall in 1880, just a year after his discovery of the ordinary Hall effect, when he observed an anomalous response in ferromagnetic iron. The modern quantum-mechanical explanation emerged in the 1980s with the concept of Berry phases applied to solid-state physics.
In a ferromagnetic material, the spin-polarized electrons experience an effective magnetic field due to spin–orbit interaction, which deflects them sideways as they move. This deflection can be understood as a Berry phase effect: the electron's wavefunction acquires a geometric phase as it traverses the crystal momentum space, leading to a transverse velocity component. The result is a Hall voltage that scales with the magnetization, even in zero applied field.
It is used in magnetic sensors, read heads for hard drives, and in research on topological materials and spintronic devices, where it enables efficient manipulation of spin currents.
The anomalous Hall effect can be so strong that in some materials, the transverse voltage is comparable to the longitudinal voltage drop, a feature exploited in compact magnetic field detectors.
| η_H | variable | Hall viscosity — hall viscosity kilogram per metre second |
| A_abcd | variable | geometric tensor — geometric tensor |
| E^ab | variable | strain tensor — strain tensor |
| ∫ dA | operator | Integration over the two-dimensional area — area integral |
| ∂_t | operator | Partial derivative with respect to time — partial time derivative |
















