A device that measures the strength and direction of magnetic fields.A magnetometer is an instrument that measures the strength and, in many cases, the direction of magnetic fields. It is one of the most versatile tools in physics, used everywhere from smartphones (for compass apps) to space probes mapping the magnetic fields of distant planets. The device works by detecting the force that a magnetic field exerts on a sensitive element, whether that element is a tiny needle, a beam of light, or a quantum defect in a diamond lattice.
The first magnetometer was the dip circle, developed in the 16th century to measure the inclination of Earth's magnetic field. Modern electronic versions emerged in the 20th century, with the fluxgate magnetometer invented in the 1930s and the SQUID in the 1960s.
Most magnetometers fall into two broad categories: scalar and vector. Scalar magnetometers measure the total magnitude of the field, often using the precession of atomic spins (like in proton precession magnetometers). Vector magnetometers, such as fluxgate or SQUID devices, measure the field's components along specific axes, revealing direction as well as strength. Newer optical techniques, like those using nitrogen-vacancy centers in diamond, exploit quantum spin states that change their fluorescence in response to magnetic fields, allowing for high-resolution imaging at the microscale.
Magnetometers are used in geophysical surveys to locate mineral deposits, in archaeology to map buried structures, in space missions to study planetary magnetic fields, and in medical diagnostics for magnetocardiography, which measures the heart's magnetic signature.
The magnetometer on the Voyager spacecraft detected that Uranus's magnetic field is tilted 59 degrees from its rotation axis, making it unlike any other planet's field in the solar system.




















