73
C H A P T E R 3
Finite Ferrite Samples
3.1 DEMAGNITIZATION FACTORS AND FERRITE
SAMPLES
In the analysis in Chapter 2, an infinitely extending ferrite material, biased by a DC magnetic
field, was considered. In turn, the permeability tensor expressions either with or without losses
are only valid for the internal fields within the ferrite and only when the alternating fields are
uniform throughout all space, e.g., Hogan [1]. However, in practice, a finite ferrite specimen is
used. e specimen can be in the form of small spheres, rods or posts, thin disks or plates as well
as in the form of thin or thick films. Films are of particular interest in the quest for miniaturiza-
tion and the integration process. Moreover, the ferrite permeability tensor is expressed in terms
of the DC biasing field
N
H
0
D
N
H
i
internal to the ferrite. e question in the finite sample case
is how this internal field
N
H
i
is related to the corresponding externally applied one
N
H
a
(which is
more readily measured), that is, the DC magnetic field in the air surrounding the ferrite sample.
e answer in principle is straightforward. Fields
N
H
a
and
N
H
i
are related through the boundary
conditions at the ferrite-air interface. However, this is not so simple since the ferrite perme-
ability involved depends on
N
H
i
. A formulation accounting for this field should be established.
A classical approach given by Kittel [2] is the introduction of demagnetization factors into the
magnetic susceptibility or permeability tensor. e demagnetization factors can be defined by
applying the boundary conditions at the ferrite-air interface. Let us first examine two special
cases of the DC biasing field orientation with respect to the ferrite sample surface. First, we as-
sume a planar sample (Figure 3.1a) transversely magnetized at saturation (
N
M D
N
M
s
) as shown in
Figure 3.1b. e continuity of the magnetic flux density normal to the planar sample component
(B
n
) yields:
B
n
D
0
H
a
D
0
.
H
i
C M
s
/
: (3.1)
In addition, the internal field becomes
H
i
D H
a
M
s
: (3.2)
Equation (3.2) shows that M
s
reduces the internal field with respect to its value in the
air region. In contrast, when a longitudinal saturation magnetization is applied, the continuity
of the tangential magnetic field
N
H
t
retains an internal magnetic field identical to the externally
applied one
N
H
a
, as shown in Figure 3.1c. In other words,
N
H
t
D
N
H
a
D
N
H
i
: (3.3)