The magnetic moment is a vector quantity that measures the strength and orientation of a magnetic source and determines how that source interacts with magnetic fields and electric currents. A simple magnetic object like a magnet or a loop of electric current, and microscopic systems such as an electron or a molecule, all possess magnetic moments. Even large bodies like a planet can be characterized by an overall magnetic moment. The direction of the magnetic moment is commonly represented as a vector, in the same way that other directional quantities in physics are treated (vectors).
Definition and basic relations
For many practical systems the magnetic moment of a current loop equals the current times the loop area and points along the loop's axis: m = I A n̂. In an external magnetic field B, a magnetic moment m experiences a torque τ given by τ = m × B and has potential energy U = −m · B. These relations explain why magnets align with external fields and why current loops produce magnetic dipole fields. The SI unit of magnetic moment is ampere-square metre (A·m²); atomic and particle physics also use characteristic units such as the Bohr magneton to compare microscopic moments.
Field pattern and multipole expansion
In space, the leading contribution of a localized magnetic source at large distances is its magnetic dipole term. The dipole component has a characteristic angular symmetry about the magnetic moment direction and falls off approximately as the inverse cube of the distance. More complicated distributions produce higher multipole contributions (quadrupole, octupole, etc.), but the dipole term often dominates at distances large compared with the source size. The dipole field is responsible for the familiar two‑pole pattern of bar magnets and planetary fields.
Classical and quantum origins
Classically, magnetic moments arise from moving electric charge: macroscopic magnets can be modeled as microscopic current loops or aligning atomic magnetic moments. Quantum mechanics adds intrinsic sources: electrons carry intrinsic spin and orbital angular momentum that produce magnetic moments not reducible to literal current loops. The electron's magnetic moment includes both spin and orbital contributions; the Bohr magneton sets the natural scale for atomic moments, while nuclear magnetic moments are typically much smaller.
Examples, scales, and distinctions
- Current loop: a textbook example where m = I A n̂ and the dipole field shape can be calculated explicitly.
- Bar magnet: behaves like a dipole at large distances with a north and south pole aligned along m; the vector commonly points from the magnet's south pole to its north pole.
- Electron and atoms: quantum moments determine atomic spectra and responses measured by techniques such as electron spin resonance.
- Planetary fields: a planet’s global dipole moment gives rise to magnetospheres and influences charged-particle dynamics in space.
Measurement and applications
Magnetic moments are measured and exploited across science and technology. Laboratory techniques include torque magnetometry, SQUID magnetometers, nuclear magnetic resonance and electron spin resonance, each sensitive to different scales. Applications range from magnetic storage and sensors to medical imaging and fundamental tests of particle and condensed-matter physics. Understanding the magnetic moment and its interaction with fields is central to designing devices and interpreting magnetic phenomena.
Notable clarifications
Magnetic moment should not be confused with magnetic field: the former is a property of a source (often summarized as a dipole vector), while the latter is the field that fills space and exerts forces and torques. Related quantities include magnetization, the magnetic moment per unit volume, and magnetic susceptibility, which describes how materials acquire induced moments in response to applied fields. For a concise visualization of a dipole and related ideas see a schematic on dipole structure; for historical and practical contexts consult entries on torque and magnetic field.

