Magnetic induction
In physics, and more in particular in the theory of electromagnetism, magnetic induction (commonly denoted by B) is a vector field closely related to the magnetic field H.
The SI unit measuring the strength of B is T (tesla), and the Gaussian unit is gauss. One tesla is 10 000 gauss. To indicate the order of magnitude: the magnetic field (or better magnetic induction) of the Earth is about 0.5 gauss = 50 μT. A medical MRI diagnostic machine typically supports a field of 2 T. The strongest magnets in laboratories are presently about 30 T.
Relation between B and H
In vacuum, that is, in the absence of a ponderable, continuous, and magnetizable medium, the fields B and H are related as follows,
where μ0 is the magnetic constant (equal to 4π⋅10−7 N/A2).
In a continuous magnetizable medium the relation between B and H contains the magnetization M of the medium,
which expresses the fact that B is modified by the induction of a magnetic moment (non-zero magnetization) in the medium.
In almost all non-ferromagnetic media, the magnetization M is linear in H,
For a magnetically isotropic medium the magnetic susceptibility tensor χ is a constant times the identity 3×3 matrix, χ = χm 1. For an isotropic medium we obtain for SI and Gaussian units, respectively, the relation between B and H,
The material constant μ, which expresses the "ease" of magnetization of the medium, is called the magnetic permeability of the medium. In most non-ferromagnetic materials χm << 1 and consequently B ≈ μ0H (SI) or B ≈ H (Gaussian).