The most important electromagnetic property of nuclei is their net charge. It is what keeps the electrons in atoms and molecules together. However, nuclei are not really electric point charges. They have a small size. In a spatially varying electric field most respond somewhat different than a point charge. It is said that they have an electric quadrupole moment. Also, most nuclei act like little electromagnets. It is said that they have a “magnetic dipole moment.” These properties are important for applications like NMR and MRI, and for experimentally examining nuclei.
This subsection explains the magnetic dipole and electric quadrupole moments from a classical point of view.
The most basic description of an electromagnet is charges going around
in circles. It can be seen from either classical or quantum
electromagnetics that the strength of an electromagnet is proportional
to the angular momentum
of the charges times the ratio of
their charge
to their mass
,
This leads to the definition of the magnetic dipole moment as
Consider a nuclear charge distribution with charge density
placed in an external electrical potential, or “voltage”
.
It may be noted that since nuclear energies are of the order of MeV,
an external field is not going to change the nuclear charge
distribution
.
Since nuclei are so small compared to normal external fields, the
electric potential
can be well represented by a Taylor
series. That gives the potential energy as
The first integral in the expression above is just the net nuclear
charge
.
-
The last integral in the expression for the potential energy defines
the quadrupole matrix or tensor. You may note a mathematical
similarity with the moment of inertia matrix of a solid body in
classical mechanics. Just like there, the quadrupole matrix can be
simplified by rotating the coordinate system to principal axes. That
rotation gets rid of the integrals
for
,
Note that the average of
,
,
is
.
is zero due to
Maxwell”s first equation, chapter 13.2. All that
then leads to a definition of an electric quadrupole moment for a
single axis, taken to be the
-
That gives
units of square length, which is easy to put in
context. Recall that nuclear sizes are of the order of a few
femtometer. So the SI unit square femtometer, ![]()
![]()
![]()
as defined. It is therefore needless to say that most sources do
not use it. They use the “barn,” a non-SI unit equal to ![]()
![]()
To better understand the likely values of the quadrupole moment,
consider the effect of the charge distribution of a single proton. If
the charge distribution is spherically symmetric, the averages of
,
and
are equal, making
zero. However,
consider the possibility that the charge distribution is not
spherical, but an ellipsoid of revolution, a “spheroid.”. If the axis of symmetry is the
-
is then about
of the
square nuclear radius
.
-
is about
of
the square nuclear radius. Either way, the values of
are
noticeably less than the square nuclear radius.
It may be noted that the quadrupole integrals also pop up in the description of the electric field of the nucleus itself. Far from the nucleus, the deviations in its electric field from that of a point charge are proportional to the same integrals, compare chapter 13.3.3.
Quantum mechanics makes for some changes to the classical description of the electromagnetic moments. Angular momentum is quantized, and spin must be included.
As the classical description showed, the strength of an electromagnet
is essentially the angular momentum of the charges going around, times
the ratio of their charge to their mass. In quantum mechanics angular
momentum comes in units of
.
and mass
.
But quantum mechanics brings in a complication, chapter
13.4. Protons have intrinsic angular momentum, called
spin. That also acts as an electromagnet. In addition the magnetic
strength per unit of angular momentum is different for spin than for
orbital angular momentum. The factor that it is different is called
the proton
-
.
![]() |
(14.27) |
Neutrons do not have charge and therefore their orbital motion creates
no magnetic moment. However, neutrons do create a magnetic moment
through their spin:
| (14.28) |
The net magnetic dipole moment operator of the complete nucleus is
![]() |
(14.29) |
Now assume that the nucleus is placed in an external magnetic field
and take the
-
However, it is not immediately clear what nuclear wave function
to use in the expectation value above. Because of the large values of
nuclear energies, a nucleus is affected very little by its
surroundings. It behaves essentially as if it is isolated in empty
space. That means that while the nuclear energy may depend on the
magnitude of the nuclear spin
,
in the
chosen
-
?
?
Now a nucleus is a composite structure, consisting of protons or
neutrons, each contributing to the net magnetic moment. However, the
protons and neutrons themselves are composite structures too, each
consisting of three quarks. Yet at normal energy levels protons and
neutrons act as elementary particles, whose magnetic dipole moment is
a scalar multiple
of their spin. Their energies in a magnetic
field split into two values, one for the state with
and the other with
.
,
.
The same turns out to be true for nuclei; they too behave as
elementary particles as long as their wave functions stay intact. In a
magnetic field, the original energy level of a nucleus with spin
splits into equally spaced levels corresponding to nuclear magnetic
quantum numbers
.
is therefore defined
to be the expectation value of
in the nuclear state in which
has its largest value
,
state:
The fact that nuclei would behave so simple is related to the fact that nuclei are essentially in empty space. That implies that the complete wave function of a nucleus in the ground state, or another energy eigenstate, will vary in a very simple way with angular direction. Furthermore, that variation is directly given by the angular momentum of the nucleus. A brief discussion can be found in chapter 7.3 and its note. See also the discussion of the Zeeman effect, and in particular the weak Zeeman effect, in addendum {A.37}.
The most important consequence of those ideas is that
Nuclei with spin zero do not have magnetic dipole moments.That is not very easy to see from the general expression for the magnetic moment, cluttered as it is with
The definition of the electric quadrupole moment follows the same
ideas as that of the magnetic dipole moment. The numerical value of
the quadrupole moment is defined as the expectation value of
,
equals the nuclear spin
:
Note that there is a close relation with the spherical harmonics;
![]() |
(14.32) |
Nuclei with spin zero or with spin one-half do not have electric quadrupole moments.To see why, note that the expectation value involves the absolute square of the wave function. Now if you multiply two wave functions together that have an angular dependence corresponding to a spin
It makes nuclei with spin
popular for nuclear magnetic
resonance studies. Without the perturbing effects due to quadrupole
interaction with the electric field, they give nice sharp signals.
Also of course, analysis is easier with only two spin states and no
quadrupole moment.
According to the odd-particle shell model, all even-even nuclei have spin zero and therefore no magnetic or electric moments. That is perfectly correct.
For nuclei with an odd mass number, the model says that all nucleons
except for the last odd one are paired up in spherically symmetric
states of zero spin that produce no magnetic moment. Therefore, the
magnetic moment comes from the last proton or neutron. To get it,
according to the second last subsubsection, what is needed is the
expectation value of the magnetic moment operator
as given
there. Assume the shell that the odd nucleon is in has
single-particle net momentum
.
.
one because the spectroscopic notation is useless as
always. In particular for an odd-even nucleus,
It is then found that for an odd proton, the magnetic moment is
Odd-odd nuclei are too messy to be covered here, even if the Nordheim rules would be reliable.
For the quadrupole moments of nuclei of odd mass number, filled shells
do not produce a quadrupole moment, because they are spherically
symmetric. Consider now first the case that there is a single proton
in an otherwise empty shell with single-particle momentum
.
The expectation value
can hardly be much more
than the square nuclear radius, excepting maybe halo nuclei. A
reasonable guess would be to assume that the proton is homogeneously
distributed within the nuclear radius
.
Next consider the case that there are not one but
3 protons
in the unfilled shell. The picture of the odd-particle shell model as
usually painted is: the first
protons are pairwise combined in
spherically symmetric states and the last odd proton is in a single
particle state, blissfully unaware of the other protons in the shell.
In that case, the quadrupole moment would self evidently be the same
as for one proton in the shell. But as already pointed out in section
14.12.4, the painted picture is not really correct. For one,
it does not satisfy the antisymmetrization requirement for all
combinations on protons. There really are
protons in the shell
sharing one wave function that produces a net spin equal to
.
In particular consider the case that there are
protons in the
shell. Then the wave function takes the form of a filled shell,
having no quadrupole moment, plus a “hole”, a state of
angular momentum
for the missing proton. Since a proton hole has
minus the charge of a proton, the quadrupole moment for a single hole
is opposite to that of one proton:
Since neutrons have no charge, even-odd nuclei would in the simplest
approximation have no quadrupole moment at all. However, consider the
odd neutron and the spherical remainder of the nucleus as a two-body
system going around their common center of gravity. In that picture,
the charged remainder of the nucleus will create a quadrupole moment.
The position vector of the remainder of the nucleus is about 1![]()
times shorter than that of the odd neutron, so quadratic lengths are a
factor 1![]()
shorter. However, the nucleus has
times as much
charge as a single proton. Therefore you expect nuclei with an odd
neutron to have about ![]()
![]()
times the quadrupole moment of the
corresponding nucleus with an odd proton instead of an odd neutron.
For heavy nuclei, that would still be very much smaller than the
magnetic moment of a similar odd-even nucleus.
For deformed nuclei, part of the angular momentum is due to rotation
of the nucleus as a whole. In particular, for the ground state
rotational band of deformed even-even nuclei, all angular momentum is
in rotation of the nucleus as a whole. This is orbital angular
momentum. Protons with orbital angular momentum produce a magnetic
dipole moment equal to their angular momentum, provided the dipole
moment is expressed in terms of the nuclear magneton
.
If a rotational band has a minimum spin
that is not zero,
the dipole moment is, [38, p. 392],
The quadrupole moment of deformed nuclei is typically many times
larger than that of a shell model one. According to the shell model,
all protons except at most one are in spherical orbits producing no
quadrupole moment. But if the nucleus is deformed, typically into
about the shape of some spheroid instead of a sphere, then all protons
contribute. Such a nucleus has a very large “intrinsic” quadrupole moment
.
However, that intrinsic quadrupole moment is not the one measured.
For example, many heavy even-even nuclei have very distorted
intrinsic shapes but all even-even nuclei have a measured
quadrupole moment that is zero in their ground state. That is a pure
quantum effect. Consider the state in which the axis of the nucleus
is aligned with the
-
-
-
A simple known system that shows such effects is the hydrogen atom.
Classically the atom is just an electron and a proton at opposite
sides of their center of gravity. If they are both on the
-
.
A model of a spheroidal nucleus produces the following relationship
between the intrinsic quadrupole moment and the one that is measured:
Figure 14.40 shows ground state magnetic moments in units
of the nuclear magneton
.
to produce the orbital momentum
.
,
One good thing to say about it all is that the general magnitude is
well predicted. Few nuclei end up outside the Schmidt lines.
(Rhodium-103, a stable odd-even
nucleus, is a notable
exception.) Also, some nuclei are actually on their line. And the
others tend to at least be on the right side of the cloud. The bad
news is, of course, that the agreement is only qualitatively.
The main excuses that are offered are:
For odd-odd nuclei, the data average out to about
nuclear
magnetons, with a standard deviation of about one magneton. These
average values are shown as yellow lines in figure 14.40.
Interestingly enough, the average is like a collective rotation,
(14.37).
According to the shell model, two odd particles contribute to the spin and magnetic moment of odd-odd nuclei. So they could have significantly larger spins and magnetic moments than odd mass nuclei. Note from the data in figure 14.40 that that just does not happen.
Even-even nuclei do not have magnetic moments in their ground state.
Figure 14.41 shows the magnetic moments of the first exited
![]()
![]()
![]()
nuclear magnetons. Bright green squares
are correct. Big deviations occur only near magic numbers. The
maximum error in the shown data is about a quarter of a nuclear
magneton, subjectively evaluated.
If you love the shell model, you may want to skip this subsection. It is going to get a beating.
The prediction of the shell model is relatively straightforward. The
electric quadrupole moment of a single proton in an unfilled shell of
high angular momentum can quite well be ballparked as
Well, you might be able to find a smaller square somewhere. For
example, the square for lithium-6, straight above doubly-magic
,
,
.
has a relatively
small square of the right color. Some nuclei on magic proton number
lines have quite small scaled quadrupole moments, though hardly almost
zero as they should. Nuclei one proton above magic proton numbers
tend to be of the right color, blue, as long as their squares are
small. Nuclei one proton below the magic proton numbers should be
red; however, promotion can mess that up.
Back to reality. Note that many nuclei in the
82,
82 wedge, and above
82, as well as various other nuclei,
especially away from the stable line, have quadrupole moments that are
very many times larger than the ballpark for a single proton. That is
simply not possible unless many or all protons contribute to the
quadrupole moment. The odd-particle shell model picture of a
spherically symmetric nuclear core plus an odd proton, and maybe a
neutron, in nonspherical orbits hanging on is completely wrong for
these nuclei. These nuclei have a global shape that simply is not
spherical. And because the shell model was derived based on a
spherical potential, its results are invalid for these nuclei. They
are the deformed nuclei that also showed up in figures 14.17
and 14.20. It is the quadrupole moment that shows that it
was not just an empty excuse to exclude these nuclei in shell model
comparisons. The measured quadrupole moments show without a shadow of
a doubt that the shell model cannot be valid.
You might however wonder about the apparently large amount in random scatter in the quadrupole moments of these nuclei. Does the amount of deformation vary that randomly? Before that can be answered, a correction to the data must be applied. Measured quadrupole moments of a deformed nucleus are often much too small for the actual nuclear deformation. The reason is uncertainty in the angular orientation of these nuclei. In particular, nuclei with spin zero have complete uncertainty in orientation. Such nuclei have zero measured quadrupole moment regardless how big the deformation of the nucleus is. Nuclei with spin one-half still have enough uncertainty in orientation to measure as zero.
Figure 14.43 shows what happens if you try to estimate the
“intrinsic” quadrupole moment of the nuclei in absence
of uncertainty in angular orientation. For nuclei whose spin is at
least one, the estimate was made based on the measured value using
(14.39), with both
and
equal to the
spin. This assumes that the intrinsic shape is roughly spheroidal.
For shell-model nuclei, this also roughly corrects for the spin
effect, though it overcorrects to some extent for nuclei of low spin.
To estimate the intrinsic quadrupole moment of nuclei with zero ground
state spin, including all even-even nuclei, the quadrupole moment of
the lowest excited ![]()
state was used. In either case,
was taken to be the spin of the ground state and
that of the excited state. Regrettably, these estimates do not make
much sense if the nucleus is not a rotating one.
Note in figure 14.43 how much more uniform the squares in the regions of deformed nuclei have become. And that the squares of nuclei of spin zero and one-half have similar sizes. These nuclei were not really more spherical; it was just hidden from experiments.
The observed intrinsic quadrupole moments in the regions of deformed nuclei correspond to roughly 20% radial deviation from the spherical value. Clearly, that means quite a large change in shape.
It may be noted that figure 14.42 leaves out magnesium-23, whose reported quadrupole moment of 1.25 barn is far larger that that of similar nuclei. If this value is correct, clearly magnesium-23 must be a halo nucleus with two protons outside a neon-21 core.