
durations, namely 9.1 ms and 15.7 ms. The increase
of the eddy current moment with decreasing pulse
duration is clearly visible. The phase shift between
magnetization and field is approximately 901. The
experimentally determined eddy currents agree well
with a Finite Element calculation. It was shown that
plotting the eddy current magnetization versus dH/dt
delivers a linear relation which can also be explained
theoretically (Gro
¨
ssinger et al. 1999).
4. The SPD method
A very important magnetic property of hard mag-
netic materials is the magneto-crystalline anisotropy
(see Magnetic Anisotropy). Generally, to investigate
this anisotropy a direction-dependent study of single
crystals is needed. In many cases such single crystals
of technically relevant materials are not available.
Often, hard magnetic materials cannot be aligned,
owing to special preparation methods. In this case the
so-called SPD method (Asti and Rinaldi 1974) is a
unique technique for determining the anisotropy.
The SPD method is based on the idea that in higher
derivatives of the magnetization with respect to the
field, d
n
M/dH
n
, a singularity appears just at that field
where H
ext
¼H
A
. In the case of a uniaxial material
the second derivative of the magnetization is already
sufficient. The amplitude of the singularity is pro-
portional to the ratio of anisotropy constants K
2
/K
1
and also proportional to the distribution function of
the crystallites. Additionally, the amplitude is deter-
mined by o
2
(H
2
max
H
2
A
). This means that a maxi-
mum external field sufficiently higher than the
anisotropy field is necessary. Moreover, the pulse
time t (oE2p=t) should be as short as possible taking
into account that the scaling is proportional to o
2
and that the noise is reduced with increasing fre-
quency. An example of the use of the SPD method is
shown in Fig. 5. It shows singularities obtained by
measurement (a) and by calculation (b) for the po-
lycrystalline Sm
2
Co
17
at room temperature. Although
the theoretical peak is sharper than that obtained by
experiment, an excellent agreement in the peak
position is observed.
The SPD method delivers the physically real
anisotropy field, H
A
, from which, knowing the sat-
uration magnetization, the technically relevant
anisotropy energy can be obtained.
See also: Magnetism: High-field; Magnetic Measure-
ments: Quasistatic and ac
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Figure 5
Measured (a) and theoretically calculated (b) singularity
of polycrystalline Sm
2
Co
17
at T ¼300 K.
496
Magnetic Measurements: Pulsed Field