In the
macroscopic formulation of electromagnetism, there appear two different kinds of
magnetic field: • the
magnetizing field H which is generated around electric currents and
displacement currents, and also
emanates from the poles of magnets. The SI units of
H are
amperes per meter. • the
magnetic flux density B which acts back on the electrical domain, by
curving the motion of charges and causing
electromagnetic induction. The SI units of
B are
volt-seconds per
square meter, a ratio equivalent to one
tesla. The concept of permeability arises since in many materials (and in vacuum), there is a simple relationship between
H and
B at any location or time, in that the two fields are precisely proportional to each other: : \mathbf{B}=\mu \mathbf{H}, where the proportionality factor
μ is the permeability, which depends on the material. The
permeability of vacuum (also known as permeability of free space) is a physical constant, denoted
μ0. The SI units of
μ are volt-seconds per ampere-meter, equivalently
henry per meter. Typically
μ would be a scalar, but for an anisotropic material,
μ could be a second rank
tensor. However, inside strong magnetic materials (such as iron, or
permanent magnets), there is typically no simple relationship between
H and
B. The concept of permeability is then nonsensical or at least only applicable to special cases such as unsaturated
magnetic cores. Not only do these materials have nonlinear magnetic behaviour, but often there is significant
magnetic hysteresis, so there is not even a single-valued functional relationship between
B and
H. However, considering starting at a given value of
B and
H and slightly changing the fields, it is still possible to define an
incremental permeability as: : \Delta\mathbf{B}=\mu \, \Delta\mathbf{H}. assuming
B and
H are parallel. In the
microscopic formulation of electromagnetism, where there is no concept of an
H field, the vacuum permeability
μ0 appears directly (in the SI Maxwell's equations) as a factor that relates total electric currents and time-varying electric fields to the
B field they generate. In order to represent the magnetic response of a linear material with permeability
μ, this instead appears as a
magnetization M that arises in response to the
B field: \mathbf{M} = \left(\mu_0^{-1} - \mu^{-1}\right) \mathbf{B}. The magnetization in turn is a contribution to the total electric current—the
magnetization current. == Relative permeability and magnetic susceptibility ==