Compute the magnetic dipole moment (μ = N·I·A) for circular or rectangular current-carrying coils. Visualize the dipole vector, determine its direction via the right‑hand rule, and calculate torque in an external magnetic field with angle dependence.
The magnetic dipole moment (μ or m) quantifies the strength and orientation of a current loop's magnetic field. For a planar coil with N turns, carrying current I, and enclosing area A, the magnitude is given by:
The direction is perpendicular to the plane of the loop, following the right‑hand rule: when fingers curl in the direction of the current, the thumb points along the dipole moment vector. In SI units, the magnetic dipole moment is measured in A·m² (ampere square meters).
The torque on a magnetic dipole in an external magnetic field B is given by the cross product:
With magnitude:
where θ is the angle between μ and B. The torque is maximum when μ ⟂ B (θ = 90°) and zero when μ ∥ B (θ = 0° or 180°). The direction is given by the right‑hand rule (perpendicular to the μ‑B plane).
For an arbitrary planar current loop, the magnetic dipole moment is defined as:
For a circular loop of radius R, this simplifies to μ = I·A with A = πR². For N turns, the contributions add linearly: μ = N·I·A.
The magnetic vector potential at a distant point (r ≫ loop dimensions) is:
| Configuration | N | I (A) | Geometry | Area (m²) | |μ| (A·m²) | Torque @ 0.5 T, 90° (N·m) |
|---|---|---|---|---|---|---|
| Small circular coil | 100 | 2.0 | R=0.05 m | 0.007854 | 1.571 | 0.785 |
| Rectangular MRI coil | 50 | 120 | 0.4×0.3 m | 0.12 | 720 | 360 |
| MEMS circular coil | 10 | 0.01 | R=0.002 m | 1.257e-5 | 1.257e-6 | 6.28e-7 |
| Physical System | Typical μ Value (A·m²) | Notes & Reference |
|---|---|---|
| Electron spin magnetic moment | 9.274×10⁻²⁴ | Bohr magneton μB |
| Proton magnetic moment | 1.4106×10⁻²⁶ | Nuclear magneton μN |
| Small bar magnet | 0.1-1 | Household magnet |
| MRI gradient coil | 10-1000 | Medical imaging |
| Earth's magnetic dipole | 8.0×10²² | Geomagnetic field source |
The Earth behaves like a giant magnetic dipole with a moment of approximately 8×10²² A·m². Our calculator cannot directly simulate planetary scales, but a theoretical loop with N=1, I≈1.73×10⁹ A and radius equal to Earth's core radius (≈3.5×10⁶ m) would produce a comparable moment. This analogy helps geophysicists model the geomagnetic field and its reversals. The torque from the solar wind interacts with Earth's dipole, creating complex magnetospheric dynamics.