
Magnetization Reversal Dynamics
Many important technological applications involve
reversing magnetic moment in a magnetic material
within a very short time period. For instance, in
computer hard-disk drives, storing a single bit re-
quires reversing the magnetic moments of both the
write transducer and the thin film recording medium
in a fraction of a nanosecond. Understanding mag-
netization reversal dynamics is critical in these appli-
cations (Bertram and Zhu 1992, Mao 2000, Zhu
2001, Zhu and Zheng 2002).
In general, magnetization reversal in a magnetic
material, either of a bulk or thin film, or a particulate
form, is always complex. For studying the reversal
dynamics, there are many experimental means, in-
cluding time-resolved Kerr microscopy field in situ
transmission electron microscopy, field in situ scan-
ning electron microscopy with polarization analysis
(SEMPA), and field in situ magnetic force microscopy
(Hubert and Scha
¨
fer 2000).
Magnetization reversal dynamics can also be stud-
ied via micromagnetic modeling. Combining the
gyromagnetic dynamic equation with the classic mi-
cromagnetic theory (Strikman and Treves 1963,
Brown 1978), the dynamic microscopic magnetiza-
tion reversal process in a ferromagnetic object can be
simulated on a computer or on a cluster of computers
(e.g., Zhu 1989). In the modeling, magnetic energy
density, E, that includes magnetocrystalline aniso-
tropy energy, magnetostatic energy, ferromagnetic
exchange energy, and magnetic potential energy
(Zeeman energy), is calculated at each location of
the object:
E ¼ E
anisotropy
þ E
magneto
þ E
exchange
þ E
Zeeman
ð1Þ
The effective magnetic field exerted on a local
magnetic moment is
H ¼
@E
@M
¼
@E
@M
x
#
e
x
þ
@E
@M
y
#
e
y
þ
@E
@M
z
#
e
z
ð2Þ
1. Gyromagnetic Equations with Energy Damping
Consider a magnetic moment with magnetization M
in a magnetic field H. Due to the fact that magnetic
moment in a magnetic material arises from electron
spin angular momentum and orbital angular mo-
mentum, the magnetic moment precesses around the
field direction, described by the following torque
equation (Landau and Lifshitz 1935):
dM
dt
¼gM H ð3Þ
where g is the gyromagnetic constant. In this process,
the angle between the magnetic moment and the field
remains unchanged. In other words, the energy of
the system is conserved. Any energy dissipation
(or often referred to as energy damping) in the sys-
tem results in a reduction of the angle. To include
energy dissipation, one phenomenological form is the
Gilbert equation:
dM
dt
¼gM H þ
a
M
M
dM
dt
ð4Þ
where M is the magnitude of the magnetic moment
and a is referred to as the damping constant (Gilbert
1955). In this form, the damping motion of the mo-
ment direction towards field direction is viscous. The
above implicit form of the dynamic equation can be
transformed into the following explicit one, known as
the Landau–Lifshitz equation (Landau and Lifshitz
1935):
dM
dt
¼g
L
M H
l
M
M M H ð5Þ
with
g
L
¼
g
1 þ a
2
and l ¼
ga
1 þ a
2
In both Gilbert and Landau–Lifshitz equations,
the magnitude of the magnetic moment is unchanged.
Under the Gilbert equation, if the energy does not
depend explicitly on time, the rate of the energy
change is given by (Zhu 1989)
dE
dt
¼m
0
ag
ð1 þ a
2
ÞM
2
7M H7
2
ð6Þ
2. Magnetization Reversal of a Uniformly
Magnetized Sphere
Consider a uniformly magnetized single-domain
magnetic sphere in a magnetic field. At nonzero
damping, the magnetic moment of the sphere rotates
towards the field direction while precessing around
the field direction. The smaller the damping constant
a, the greater the number of precession cycles will be
before the magnetic moment aligns with the field di-
rection. Figure 1 shows the calculated trajectories
according to Eqn. (4) for two different values of the
damping constant a. The time duration of the re-
versal, from near antiparallel direction to the parallel
direction, with respect to the field is given by
Dt ¼
1 þ a
2
agðH2H
s
Þ
ln
tanðy
2
=2Þ
tanðy
1
=2Þ
ð7Þ
where y
2
and y
1
are the final and initial angles be-
tween the magnetic moment and the field whose am-
plitude is denoted by H, and H
s
is the switching field
threshold (e.g., the anisotropy field). For a given
magnetic field whose amplitude is greater than the
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Magnetization Reversal Dynamics