
R(t)—is not an infinitely sharply determined quanti-
ty. Small intrinsic effects, such as vibrational motion
of the probe atom, can cause slight changes in the
environments, which will show up as a damping of
R(t) described by mainly Lorentzian or Gaussian
distributions on the frequencies in its Fourier spec-
trum. For such intrinsic effects, the damping is gen-
erally very weak. If, however, severe perturbations
of the environments are present, e.g., lattice defects,
vacancies, impurities, R(t) will die out much faster.
Determining the amount of distribution can therefore
tell how pure the environment of the probe is on
the atomic scale. Another use of the distribution is
discussed in Sect. 6.
5. Theoretical Understanding of Hyperfine Fields
A very important problem when using any nuclear
technique is to relate a measured hyperfine field
(which is a very local quantity) to particular chemical
and physical properties of the neighborhood of the
probe nucleus, and even of the material as a whole.
This problem was for long dealt with in a rather
crude, phenomenological way. It took until the early
1990s to be solved, when ab initio methods with
quantitative predicting power were developed. Major
work was carried out by Blaha et al. (1999) within
the framework of density functional theory (DFT,
see Density Functional Theory: Magnetism). By using
the full potential felt by the electrons and solving
the resulting Kohn–Sham equation by the linearized
augmented plane wave (LAPW) method, the tails of
the electron wave functions near the nucleus can be
calculated with a sufficient accuracy to obtain the
hyperfine field. The method has been implemented
in the computer code WIEN, which is a standard
tool for calculating hyperfine fields in a variety of
materials.
6. Example
To illustrate PAC measurements, thin Fe/Cr multi-
layers are discussed as a case study (Meersschaut
et al. 1995).
Bulk b.c.c. chromium is known to have an exotic
type of antiferromagnetic order: a spin density wave
(SDW). The moments are oriented along the 100 di-
rection and moments at neighboring atoms are an-
tiparallel. But instead of displaying the same
magnitude of moment everywhere in the crystal, as
is usual in an antiferromagnet, in chromium the mo-
ment magnitude is sinusoidally modulated with a pe-
riod of approximately 20 lattice units. Between 311K
and 123K the moments are perpendicular to the
propagation direction of the wave (transverse SDW).
Below 123K the moments are parallel to the prop-
agation direction (longitudinal SDW).
An interesting question as to the magnetic order
and the character of the SDW arises when thin chro-
mium layers are considered with a thickness ap-
proaching the period of the SDW. Will the SDW
survive or not? If so, will it be transverse or longi-
tudinal? Will the chromium moments keep their orig-
inal 100 direction? To examine this,
111
In nuclei were
implanted into a multilayer containing several Fe/Cr
bilayers, grown with the 100 direction perpendicular
to the layer. The
111
In probe atom is known to take
substitutional lattice sites in both the chromium and
iron layers, where they decay with a lifetime of 2.81
days into the PAC nucleus
111
Cd. The latter nucleus
interacts with a hyperfine field generated by the sur-
rounding cadmium electrons, which is directed along
the cadmium moment (the moment of the diamag-
netic cadmium atom is induced by, and hence is par-
allel to, the surrounding chromium moments).
The R(t) function of two PAC measurements is
shown in Fig. 1. In Fig. 1(a) the multilayer is parallel
to the detector plane and in Fig. 1(b) it is perpendic-
ular to it. In both R(t) functions contributions from a
slow and a fast frequency are visible. The slow fre-
quency belongs to
111
Cd nuclei in a chromium envi-
ronment and the fast one to an iron environment.
The line through the data points is a best fit, with the
chromium contribution to it shown in the lower
curves. From the change in frequencies when the
multilayer is tilted from Figs. 1(a) to (b), it can be
deduced that the hyperfine field on cadmium in chro-
mium—and therefore the chromium magnetization—
is oriented perpendicular to the plane of the multi-
layer, and hence along the 100 direction. Moreover,
the R(t) function belonging to chromium positions is
not a pure sine wave but a Bessel function. Theory
shows that this typical shape appears when the nuclei
each experience a different hyperfine field corre-
sponding to an Overhauser distribution in frequency
space and a sine wave in real space: solid proof that
the SDW is present in this type of Fe/Cr multilayer.
Furthermore it has been shown—first by PAC and
later by neutron scattering and transport methods—
that the SDW is longitudinal and disappears below a
critical chromium thickness.
See also:Mo
¨
ssbauer Spectrometry; Nuclear Mag-
netic Resonance Spectrometry
Bibliography
Blaha P, Schwarz K, Luitz J 1999 WIEN97, A Full Potential
Linearized Augmented Plane Wave Package for Calculating
Crystal Properties. Karlheinz Schwarz, Vienna (updated ver-
sion of Blaha P, Schwarz K, Sorantin P, Trickey S B Comp.
Phys. Commun. 59, 399–415)
Cahn R W, Lifshin E 1993 Concise Encyclopedia of Materials
Characterization. Pergamon, Oxford, UK
Catchen G L 1995 PAC: renaissance of a nuclear technique.
MRS Bull. (July), 37–46
1051
Perturbed Angular Correlations (PAC)