
A dimensionless quantity indicating how much a material becomes magnetized in an applied magnetic field.Magnetic susceptibility is a dimensionless quantity that measures how strongly a material responds to an applied magnetic field. It tells you whether a material will be attracted to a magnet (paramagnetic), repelled by it (diamagnetic), or retain magnetization after the field is removed (ferromagnetic). The value is defined as the ratio of the magnetization produced in the material to the applied magnetic field strength, and it can be positive, negative, or even zero.
The concept was formalized in the 19th century, with key contributions from Michael Faraday, who studied magnetic induction in various substances, and later by Pierre Curie, who established the temperature dependence for paramagnets.
When an external magnetic field is applied, it aligns the magnetic moments of atoms or electrons within the material. In paramagnetic materials, the alignment is weak and temporary, giving a small positive susceptibility. In diamagnetic materials, the field induces opposing magnetic moments, yielding a small negative susceptibility. Ferromagnetic materials have domains that align strongly and can retain alignment, giving large positive values that depend on the material's history.
It is used in materials science to classify substances, in magnetic resonance imaging (MRI) to enhance contrast, and in geophysics to map underground mineral deposits.
Water has a negative magnetic susceptibility, which is why a strong magnet can make a frog levitate — the water in its body is diamagnetically repelled.

