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Basic Theory
Nuclear magnetic resonance (NMR) is a very subtle technique which uses the
spin of the nuclei as a probe for their environment. Nuclear magnetic
resonance therefore can be used for measuring many microscopic
properties of solids.
While nuclear spin resonance takes advantage of the lifted degeneracy
of a nuclear spin in an external magnetic field, in nuclear quadrupolar
resonance this degeneracy is lifted by the interaction of the
quadrupolar momentum of the core with its environment. But the discussion
of the contributions to the hamiltonian of a spin in a solid can
be found in another chapter of this work. Here we want to restrict
our attention to the terms which are of a technical interest.
In nuclear spin resonance one applies a static field in the
z-direction and a rf field in the x-y-plane. The terms have the
form:
with
the nuclear gyromagnetic ratio,
the static magnetic field,
the spin operator, Ix its
x-component, B1 the amplitude of the rf field and
its
frequency.
For the time being we would like to restrict our attention to the first
of these two terms, which are -- apart from the
--
orders of magnitude larger than the others. Our first goal is now to
describe the dynamics of a non-interacting spin system affected only
by ( ). This has been done by many authors
[#!abragam!#,#!slichter!#] and I will only give a rough outline.
As one knows from quantum mechanics the state
of a
spin in an external magnetic field can be described by a projection operator
on an eigenstate of the hamiltonian ( ):
 |
(2.3) |
The time evolution of this operator is then given by
 |
(2.4) |
The problem of solving Schrödinger's equation is now reduced to
the evaluation of the expression ( ). This has been done for
example in [#!kind!#]. In considering only the Zeemann interaction
one obtains the expectation values
They are rotating around the z-axis with the larmor frequency
given by the external static field.
Therefore one can take the Zeemann part of the hamiltonian into
account by simply changing into a coordinate system which rotates with the same
frequency around the z-axis.
It is now easy to generalize to a system of N identical, non-interacting
spins. Its density operator takes the form
 |
(2.7) |
Since also in an ensemble the expectation values of an operator on
a single spin depend only on the density operator of this spin
 |
(2.8) |
where we have defined the density matrix
to be the average over
all spins of the density operator of a single spin:
 |
(2.9) |
With
we can again solve our equation of motion
.
But we should
recall the fact that there are many mechanisms such as local field fluctuations
which may slowly destroy the phase coherence of the spin ensemble.
The characteristic time scale in which this coherence decays is usually shorter than T2,
the characteristic time of the spin-spin-interactions.
Therefore equation ( ) only holds for a short time ,
when there is no significant loss of phase coherence, or for a long time when we
have completely arbitrary phases (random phase approximation, RPA).
With the first assumption one replaces
of ( )
and ( ) by the ensemble average and obtains again the
oscillating off-diagonal elements. In the RPA the off-diagonal
elements vanish anyway.
We now want to apply the rf field to the spin system which means that we start to take
( ) into account. But we don't want to go through all of the formalism, instead
we'll just quote the results as they are obtained for example in [#!kind!#]:
In the case of resonant irradiation,
,
the expectation values
of the spin operators behave in such a way that the magnetisation in the rotating
coordinate system behaves like
| Mz |
= |
 |
(2.10) |
| Mx' |
= |
0 |
(2.11) |
| My' |
= |
 |
(2.12) |
with
.
It is therefore easily possible to bring the whole
magnetisation into the x-y-plane by applying an rf-pulse of the right
amplitude and the right duration. This magnetisation decays with a time constant
smaller than T2 as the spins are getting out of phase. The origin of this
decay are the local fluctuations in the magnetic field which causes the individual
larmor frequencies to deviate from the average larmor frequency.
Contrarily to the slower process of the spin-spin-interactions the decay caused by
different larmor frequencies is completely reversible. A very popular pulse
sequence which uses this fact is the so called spin echo. It is a sequence
of two pulses. It is best understood in a classical picture where we describe
the spins as magnetic momenta. The first pulse (
-pulse) then brings
the magnetization into the x-y-plane. The second pulse ( -pulse) -- which comes
after a time called
-- reflects all the momenta at the origin; an echo
after another interval
will be the answer of the spin system to this
sequence.
Figure:
(a) M0 is in thermal equilibrium lying along the z-direction,
(b) magnetization immediately after a
-pulse,
(c) an element of magnetization
has precessed
an extra angle owing to the magnetic field inhomogeneity,
(d) effect of a -pulse,
(e) at time
all elements of the magnetization have
refocused along the +y-direction.
image source: [#!slichter!#], p. 41
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In a quantum mechanical picture of energy levels one is inducing transitions
between different energy levels by irradiating the spin system with the
frequency
.
Therefore the echo intensity is proportional
to the number of transitions (spins) with this transition frequency. But in
pulsed NMR, as we do it in our laboratory, it is, due to the uncertainty principle,
no longer possible to irradiate with a well-defined frequency. The resolution
is limited by
,
where
is the
duration of the longer of the two pulses in an echo sequence for the longer
pulse makes the preciser selection in frequency.
With this knowledge it is possible to measure spectra, which may be a very
helpful tool to interpret contributions to the total hamiltonian. Unfortunately
it can also be quite difficult to separate single effects which form a spectrum.
We will come back to this later. At the moment we quickly pay some attention to
two more dynamical and easily to measure properties of a spin in a solid.
We already introduced the spin-spin-ralaxation rate T2. It is the characteristic
time during which the magnetization in the x-y-plane gets irreproducibly
lost. It's therefore the time constant with which the echo intensity decays as a
function of
(of length of the second pulse). This can very
easily be measured.
There is another governing time constant in a spin system. It is called T1,
the spin-lattice-relaxation rate. It is the time during which the spin system
relaxes to thermal equilibrium with the lattice after a perturbation. In
order to measure T1 one again takes advantage of the fact that the echo
sequence only measures one single level. If this level is empty, there will be
no echo. Figure shows an outline of how a T1-measurement
has do be designed. But we will go into detail later.
Figure:
typical pulse sequence for a T1-measurement:
first one destroys all the magnetization with the comb
sequence; after the recovery time one measures with
a normal echo sequence how much of the magnetization
is already restored.
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In usual solids T1 is much larger than T2. That means that
the hamiltonian describing the lattice almost commutes with the hamiltonian
describing the spin system. It is then often convenient to describe the total
system by more than one temperature. The irradiation of a comb sequence is then
equivalent to only heating the spin system [#!kind!#].
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