Page 269 - Engineering Electromagnetics, 8th Edition
P. 269

CHAPTER 8   Magnetic Forces, Materials, and Inductance    251

                     The magnetization is M = χ m H,or39, 000 A/m. The alternate ways of relating B
                     and H are, first,

                                                B = µ 0 (H + M)
                     or
                                                      −7
                                         0.05 = 4π × 10 (796 + 39, 000)
                     showing that Amperian currents produce 49 times the magnetic field intensity that
                     the free charges do; and second,

                                                  B = µ r µ 0 H
                     or
                                          0.05 = 50 × 4π × 10 −7  × 796

                     where we use a relative permeability of 50 and let this quantity account completely
                     for the notion of the bound charges. We shall emphasize the latter interpretation in
                     the chapters that follow.


                         The first two laws that we investigated for magnetic fields were the Biot-Savart
                     law and Amp`ere’s circuital law. Both were restricted to free space in their application.
                     We may now extend their use to any homogeneous, linear, isotropic magnetic material
                     that may be described in terms of a relative permeability µ r .
                         Just as we found for anisotropic dielectric materials, the permeability of an
                     anisotropic magnetic material must be given as a 3 × 3 matrix, and B and H are
                     both 3 × 1 matrices. We have

                                          B x = µ xx H x + µ xy H y + µ xz H z
                                          B y = µ yx H x + µ yy H y + µ yz H z
                                          B z = µ zx H x + µ zy H y + µ zz H z

                     For anisotropic materials, then, B = µH is a matrix equation; however, B =
                     µ 0 (H + M) remains valid, although B, H, and M are no longer parallel in general.
                     The most common anisotropic magnetic material is a single ferromagnetic crystal,
                     although thin magnetic films also exhibit anisotropy. Most applications of ferromag-
                     netic materials, however, involve polycrystalline arrays that are much easier to make.
                         Our definitions of susceptibility and permeability also depend on the assumption
                     of linearity. Unfortunately, this is true only in the less interesting paramagnetic and
                     diamagnetic materials for which the relative permeability rarely differs from unity
                     by more than one part in a thousand. Some typical values of the susceptibility for
                                                                           −5
                                                          −5
                     diamagnetic materials are hydrogen, −2 × 10 ; copper, −0.9 × 10 ; germanium,
                             −5
                                               −5
                                                                    −5
                     −0.8 × 10 ; silicon, −0.3 × 10 ; and graphite,−12 × 10 .Several representative
                                                           −6
                                                                            −5
                     paramagnetic susceptibilities are oxygen, 2×10 ; tungsten, 6.8×10 ; ferric oxide
                                   −3
                                                                    −6
                     (Fe 2 O 3 ), 1.4 × 10 ; and yttrium oxide (Y 2 O 3 ), 0.53 × 10 .Ifwe simply take the
                     ratio of B to µ 0 H as the relative permeability of a ferromagnetic material, typical
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