
Giant Magnetoresistance
The resistance of a ferromagnetic metal changes when
one applies a magnetic field. This change is related to
the dependence of the resistance on the angle between
the magnetization of the ferromagnet and the electri-
cal current direction, and is called anisotropic
magnetoresistance (AMR) (see Magnetoresistance,
Anisotropic). Although AMR in ferromagnets does
not exceed a few percent at room temperature, it is
used in a number of devices, mainly because the mag-
netization of a soft ferromagnetic material can be
easily manipulated in a low magnetic field. Giant
magnetoresistance (GMR) is another type of magne-
toresistance (MR) which is observed in magnetic
multilayers and is much larger than the AMR of
the ferromagnetic metals. It was discovered in 1988
(Baibich et al. 1988, Binash et al. 1989) on Fe/Cr
multilayers (stack of Fe and Cr layers) and Fe/Cr/Fe
trilayers. In these structures and at zero magnetic
field, the magnetizations of adjacent Fe layers are
oriented in opposite directions by antiferromagnetic
coupling across Cr (Gru
¨
nberg et al. 1986); when an
applied field aligns these magnetizations in parallel,
the resistance of the multilayer decreases dramatically
and this effect has been called giant magnetoresistance
(GMR). The GMR of multilayers is thus associated
with a change of the relative orientation of the mag-
netization in consecutive magnetic layers. Since this
pioneering work on exchange coupled multilayers,
GMR has been observed in a number of magnetic
nanostructures, including uncoupled multilayers, spin
valve structures, multilayered nanowires, and granu-
lar systems (for an extensive review see Barthe
´
le
´
my
et al. 1999). In multilayers, GMR has been observed
either for current in plane (CIP) or with current per-
pendicular to the plane of the layers (CPP geometry).
CPP GMR has revealed interesting spin accumulation
effects which form the basis for further developments.
From the point of view of applications, GMR is
already used in various types of devices such as sen-
sors, read-heads, and magnetic memories (MRAM).
Reading information from a hard disk, for example,
is done in many computers by detecting the resistance
change induced by the small field (about 10
3
T)
generated by the disk. This was achieved with AMR
at the beginning of the 1990s and subsequently with
GMR. While comparable fields can activate both
AMR and GMR devices, the amplitude of GMR is
larger, which permits a reduction of the size
of the information bits and an increase of the den-
sity of stored information to 10–20 gigabitsin
2
(1.6–3.1 gigabitscm
2
).
This article gives an experimental review of GMR.
First, we describe the effects observed in multilayers
(Sect. 1) or spin valve structures (Sect. 2) when the
current flows parallel to the layers. In Sect. 3 the case
where the current flows perpendicular to the layers is
discussed. In Sect. 4 we give a brief phenomenological
overview of the physics of GMR. The theoretical
models for the CIP and CPP geometries are summa-
rized in Sect. 5. Finally, inverse GMR and GMR of
granular structures are presented in Sects. 6 and 7.
1. CIP GMR in Magnetic Multilayers
GMR was first observed in Fe/Cr superlattices
(Baibich et al. 1988) and in Fe/Cr/Fe trilayers
(Binash et al. 1989), in both cases for samples grown
by molecular beam epitaxy (MBE). Figure 1 shows
the variation of resistance as a function of magnetic
field for Fe/Cr superlattices at 4.2 K. As the magnetic
field increases, the magnetic configuration of neigh-
boring iron layers goes from antiparallel to parallel.
A field H
s
is needed to overcome the antiferro-
magnetic coupling and saturate the magnetization.
Between zero field and H
s
, the resistance drops sig-
nificantly as a result of GMR. The MR ratio is de-
fined as the ratio of the resistivity change to the
resistivity in the parallel configuration. It reaches 79%
at 4.2 K for the sample in Fig. 1 with 9 A
˚
thick chro-
mium layers (and is still 20% at room temperature).
For the Fe/Cr system, the GMR ratio can reach 220%
Figure 1
MR of Fe/Cr multilayers at 4.2 K (after Baibich et al.
1988).
G
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