The polarizabilityα of a small dielectric body (e.g. an atom or molecule)
is defined to relate the electric fieldE
applied to that body to the resulting dipole moment p:
p=αε0E
If there are N such bodies per unit volume,
the polarization density P=ε0χeE
with P=Np suggests that χe=Nα.
However, this is an underestimation:
each body’s induced dipole creates its own electric field,
weakening the field felt by its neighbors.
We need to include this somehow,
but α is defined for a single dipole in a vacuum.
Let Eint be the uniform internal field excluding the dipoles’ contributions,
and E(r) the net field including them.
Assume that the dipoles pi are arranged
in a regular crystal lattice at sites Ri.
Then E(r) is the sum of Eint and all the dipoles’ fields:
E(r)=Eint+i∑Ei(r−Ri)
Where the individual contribution Ei(r)
of each dipole pi is as follows:
Ei(r)=−4πε01∇(∣r∣2r^⋅pi)
The atoms or molecules pi need not be perfect dipoles,
as long as they approximate one when viewed from a distance
much smaller than the crystal’s lattice constant.
Clearly, in a multipole expansion
of the true charge distribution ρi(r)’s electric potential Vi(r),
the dipole term will be dominant in that case, given by:
Vi(r)≈4πε01∣r∣21∫−∞∞ρi(r′)∣r′∣cosθdr′
Where θ is the angle between r and r′,
so this can be rewritten as a dot product
with the unit vector r^, normalized from r:
Vi(r)=4πε01∣r∣21r^⋅∫−∞∞r′ρi(r′)dr′
The integral is a more general definition of the dipole moment pi.
You can convince yourself of this by defining ρi(r)
as two opposite charges +q and −q
respectively located at +di/2 and −di/2;
evaluating the integral then yields qdi=pi.
Therefore:
Vi(r)=4πε01∣r∣2r^⋅pi
Then the corresponding electric field Ei is given by −∇Vi as is well known.
The dipole p0 at r=0
feels a net local field Eloc, given below.
The crystal’s symmetry ensures that all its neighbors’ fields cancel out:
since Ei(−r)=−Ei(r),
each dipole has a counterpart with the exact opposite field.
We exclude the singular term E0(0):
Eloc≡E(0)=Eint+i=0∑Ei(−Ri)=Eint
Even if there is no regular lattice, this result still holds well enough,
as long as the dipoles are uniformly distributed over a large volume.
So what was the point of including Ei(r) in the first place?
Well, keep in mind that the sum over neighbors is nonzero for r=Ri,
which does affect the macroscopic field E, defined as:
E=Eloc+Ω1∫Ωi∑Ei(r−Ri)dr
Where Ω is an arbitrary averaging volume,
large enough to contain many dipoles,
and also small enough to assume that the polarization is uniform within.
Thanks to linearity and symmetry,
we only need to evaluate this volume integral for a single dipole:
Where we have used the divergence theorem.
Let us define Ω as a sphere with radius R centered at r=0.
In spherical coordinates,
the surface integral then becomes:
The radial coordinate disappears, so in fact the radius R is irrelevant.
We choose our coordinate system such that pi points
in the positive z-direction, i.e. pi=(0,0,∣pi∣), leaving:
Experimentally, εr can be measured directly, but α cannot.
By isolating εr for Nα,
we finally arrive at the Clausius-Mossotti relation for calculating α:
31Nα=εr+2εr−1
Since many theoretical models only calculate α
(e.g. the Lorentz oscillator model),
this result is useful for relating theory to experimental results.
References
M. Fox,
Optical properties of solids, 2nd edition,
Oxford.