In a transverse field SR experiment, one measures the internal magnetic
field distribution of a superconductor in the vortex state.
Prior to the development of this technique, the internal field distribution
could be studied with NMR, which in principle provides the same
information as
SR.
The basic principles of the NMR technique are as follows:
The interaction of the magnetic moment of a nucleus
(where
is a
nonzero nuclear spin and
is the gyromagnetic ratio characteristic
of the nucleus) with the local magnetic
field
at its site is described by the Hamiltonian
![]() |
(1) |
![]() |
(2) |
![]() |
(3) |
An NMR technique which is a close parallel to SR is
``pulsed NMR'', in which one observes time-dependent transverse
nuclear polarization or so-called
``free induction decay'' of the nuclear polarization.
In this form of NMR, an RF pulse
is applied to rotate the nuclear spins
from the
direction of the local magnetic field
. When the RF
field is switched off, the nuclear spins perform a free precession
around the local field
and relax back to their initial
direction along
. The precession is detected by a
pickup coil. The frequency of the nuclear spin precession is
a measure of the local field (i.e.
).
In this pulsed NMR technique, the different precession frequencies
are observed simultaneously without variation of the RF or DC
magnetic fields [44].
However, there are several limitations and added
difficulties associated with the NMR technique which are overcome in
a
SR experiment.
The first problem is that because the skin depth of the RF field probe is small, NMR only probes the surface of the sample. For most high-Tc samples, the surface has many imperfections, which results in strong vortex-line pinning and a highly disordered vortex lattice--a topic which will be discussed in the next section. To measure the field distribution in the bulk, magnetically aligned powders are often used (see for example Ref. [51]). However, the vortex-lattice structure in the bulk of a small crystallite is also likely to be affected by the strong pinning of the vortices at the crystallite surface. Furthermore, it is difficult to align all of the crystallites with the applied field. Due to mass anisotropy, the field distribution will not be the same in crystallites with different orientations. To account for the misaligned fraction, one must measure the NMR spectrum before and after alignment, and then subtract out the random powder contribution by using a predetermined percentage of alignment. The penetration depth of the RF field also limits the range over which the vortex lattice can be sampled.
On the other hand, SR is a bulk probe
that is easily performed on
single crystals, so that one can measure the ``true'' magnetic field
distribution in the bulk. The importance of having this capability
will become clear when the structure of the vortex-lattice is
discussed in some detail later in this thesis.
Other problems with NMR are the additional sources
of line broadening in the measured internal field distribution
(i.e. line broadening sources which are negligible in SR).
For instance, in the high-Tc
materials the linewidths originating from the copper and oxygen nuclei
are very broad due to quadrupole interactions and chemical
shifts (or metallic Knight shifts).
A field distribution which corresponds more closely
to that of the vortex lattice is obtained with the
SR technique.
Since the muon is a spin 1/2 particle, it has no quadrupole
interaction.
Also,
SR is sensitive over relaxation times as small
as 10 ns compared to
s for NMR. The signal
relaxation in
SR due to the inhomogeneous field distribution of the
vortex lattice typically occurs over the first few
s.