Coercivity in a
ferromagnetic material is the intensity of the applied
magnetic field (
H field) required to demagnetize that material, after the magnetization of the sample has been driven to
saturation by a strong field. This demagnetizing field is applied opposite to the original saturating field. There are however different definitions of coercivity, depending on what counts as 'demagnetized', thus the bare term "coercivity" may be ambiguous: • The
normal coercivity, , is the
H field required to reduce the
magnetic flux (average
B field inside the material) to zero. • The
intrinsic coercivity, , is the
H field required to reduce the
magnetization (average
M field inside the material) to zero. • The
remanence coercivity, , is the
H field required to reduce the
remanence to zero, meaning that when the
H field is finally returned to zero, then both
B and
M also fall to zero (the material reaches the origin in the hysteresis curve). The distinction between the normal and intrinsic coercivity is negligible in soft magnetic materials, however it can be significant in hard magnetic materials. The strongest
rare-earth magnets lose almost none of the magnetization at
HCn. ==Experimental determination==