This addendum is concerned with vector particles, particles whose wave
functions are vectors. To be sure, the wave function of an electron
can also be written as a vector, chapters 3.1 and
5.5.1:
To really appreciate this addendum, you may want to read the previous
addendum {A.19} first. In any case, according to
that addendum angular momentum is related to what happens to the wave
function under rotation of the coordinate system. In particular, the
angular momentum in the
-
-
Consider first the simplest possible vector wave function:
![]() |
The factor
does not change under rotations because the distance
from the origin does not. But the vector
does
change. Figure A.8 shows what happens. The vector in the
rotated coordinate system
has components
Now consider three very special vectors:
The vector
has only a
-
.
zero, as the superscript in
says. Then the
angular momentum in the
-
changes by a factor
under rotation, so it has
1
-![]()
.
To get at square angular momentum, first the operator
of spin
angular momentum around the
-
Of course, the operators
and
are defined
similarly. There is nothing special about the
-
That then means that the spin
of vector particles is equal to 1.
So a vector particle is a boson of spin 1. The subscript on the
special vectors
indicates their spin
1.
You can write the most general vector wave function in the form
Like the electron, the vector particle can of course also have orbital
angular momentum. That is due to the coefficients
in the
wave function above. So far it has been assumed that these
coefficients only depended on the distance
from the origin.
However, consider the following more general component of a vector
wave function:
The wave function (A.84) above has orbital angular momentum
in the
-
in addition to the spin
angular momentum
.
-
.
while the spherical harmonic changes by
an additional factor
.
.
In general, then, the magnetic quantum number
of the net
angular momentum is simply the sum of the spin and orbital ones,
However, the situation for the azimuthal quantum number
of the net
angular momentum is not so simple. In general the wave function
(A.84) above will have uncertainty in the value of
.
.
That is a complicated issue best left to chapter 12.
But a couple of special cases are worth mentioning already. First, if
1 and
,
1
![]()
,
is simply the sum of
the spin and orbital azimuthal quantum numbers
.
The other special case is that there is zero net angular momentum.
Zero net angular momentum means that the wave function is exactly the
same regardless how the coordinate system is rotated. And that only
happens for a vector wave function if it is purely radial:
The above state has zero net angular momentum. The question of
interest is what can be said about its spin and orbital angular
momentum. To answer that, it must be rewritten in terms of Cartesian
components. Now the unit vector
has Cartesian components
The bottom line is that by combining states of unit spin
1,
and unit orbital angular momentum
1, you can create a state
of zero net angular momentum,
0. Note also that in each of
the three terms in the right hand side above,
and
add up
to zero. A state of zero angular momentum
0 must have
0 without uncertainty. Further note that the values of both the
spin and orbital angular momentum in the
-
,![]()
![]()
.
The above relation may be written more neatly in terms of “ket
notation.” In ket notation, an angular momentum state with
azimuthal quantum number
and magnetic quantum number
is
indicated as
.
,
There is a quicker way to get this result than going through the above
algebraic mess. You can simply read off the coefficients in the
appropriate column of the bottom-right tabulation in figure
12.6. (In this figure take
to stand for spin,
for
orbital, and
for net angular momentum.) Figure 12.6
also has the coefficients for many other net spin states that you
might need. A derivation of the figure must wait until chapter
12.
The parity of vector wave functions is also important. Parity is what
happens to a wave function if you invert the positive direction of all
three Cartesian axes. What happens to a vector wave function under
such an inversion can vary. A normal, or “polar,” vector changes sign when you invert the axes. For
example, a position vector
in classical physics is a polar
vector. Each position coordinate
,
,
changes sign, and therefore so does the entire vector. Similarly, a
velocity vector
is a polar vector; it is just the time
derivative of position. A particle with a vector wave function that
behaves like a normal vector has negative intrinsic parity. The sign
of the wave function flips over under axes inversion. Particles of
this type turn out to include the photon.
But now consider an example like a classical angular momentum vector,
.
Note however that the orbital angular momentum of the particle also
has an effect on the net parity. In particular, if the quantum number
of orbital angular momentum
is odd, then the net parity is the
opposite of the intrinsic one. If the quantum number
is even,
then the net parity is the intrinsic one. The reason is that
spherical harmonics change sign under spatial inversion if
is odd,
but not when
is even, {D.14}.
Particles of all types often have definite parity. Such a particle
may still have uncertainty in
.
will need to be all even or all odd.