(Ordinary ray / Extraordinary ray / Circularly polarized light)
In this
section, Feynman discusses ordinary ray
(o-ray), extraordinary ray (e-ray),
and circularly polarized light. Simply phrased, o-ray and e-ray are
symmetrical ray (spherical wavefronts) and asymmetrical ray (elliptical
wavefronts), respectively, in a birefringent crystal. In a sense, o-ray and e-ray are the same
light waves, but the interactions of the two perpendicularly polarized light with matter (or refractive
index) are different.
1. Ordinary ray:
“…When
this beam strikes the surface of the material, each point on the surface acts
as a source of a wave which travels into the crystal with velocity v⊥,
the velocity of light in the crystal when the plane of
polarization is normal to the optic axis. The wavefront is just the
envelope or locus of all these little spherical waves, and this
wavefront moves straight through the crystal and out the other side. This is
just the ordinary behavior we would expect, and this ray is called the ordinary
ray (Feynman et al., 1963, p. 33–9).”
Feynman’s definition of o-ray can be analyzed from
the perspective of optic axis, speed of light, and wavefront. Firstly, o-ray
propagates in a birefringent crystal whereby
its electric fields (plane of polarization) oscillate perpendicular to the optic
axis and direction of incident ray. Secondly, o-ray moves at a constant speed, v⊥,
which is dependent on the crystal’s refractive index (See Fig. 1). Thirdly, the wavefronts are
spherical because of the constant speed of light and same refractive index
within the crystal. However, o-ray should also be defined in terms of Snell’s
law of refraction because it obeys the equation n1sin q1 = n2sin q2 in which n1 and n2 are the refractive index of the respective medium, whereas q1 is the angle of incidence and q2 is the angle of refraction.
![]() |
Fig. 1 |
The concept of o-ray in optics is based on idealizations and
approximations of a birefringent crystal. We idealize the crystal as free of any defects or
impurities that could affect the light to deviate from its expected behavior.
In the real world, all materials have some degree of imperfections that can
cause the light passing through them to scatter, diffract, or absorb in unexpected
ways. Essentially, the o-ray is a symmetrical ray (spherical wavefronts)
oscillating perpendicular to the optic axis (approximate axis of symmetry) and experiences
almost the same refractive index. If the z-axis is the direction
of incident ray, we may assign the x-axis such that the plane of
polarization of o-ray, xz-plane, is perpendicular to the plane that contains
the incident ray and optic axis. On the contrary, we may assign the y-axis
such that the plane of polarization of e-ray, yz-plane, contains the incident ray
and optic axis.
“Anomalous refraction comes
about when the optic axis, the long axis of our asymmetric molecules, is not
parallel to the surface of the crystal (Feynman et al., 1963, p. 33–9).”
It is not generally true that anomalous refraction definitely comes
about when the optic axis is not parallel to the surface of the crystal (during
normal incidence). Note that the condition “perpendicular to the surface of the
crystal” is a special case of “not parallel to the surface of the crystal.” That
is, we cannot observe anomalous refraction when the optic axis is perpendicular
to the surface of the crystal. On the other hand, anomalous refraction is also observable
when the optic axis is parallel to the surface of the crystal (for
incoming light) or lies in the plane of the paper (as stated in Fig. 33-7). To
be precise, anomalous refraction cannot be observed when the incident ray is
parallel to the optic axis of the crystal. This is because the
refractive index of the crystal varies with the angle between the incident ray
and optic axis.
2. Extraordinary ray:
“The
envelope of all these elliptical waves is the wavefront which proceeds
through the crystal in the direction shown. Again, at the back surface the beam
will be deflected just as it was at the front surface, so that the light
emerges parallel to the incident beam, but displaced from it. Clearly, this beam does not
follow Snell’s law, but goes in an extraordinary direction. It is
therefore called the extraordinary ray (Feynman et al., 1963, p. 33–9).”
Feynman’s explanation of extraordinary ray is potentially
misleading because it is not generally true that v∥ < v⊥ in a birefringent crystal. However, we can also
define e-ray ray from three perspectives, optic axis, speed of light, and
wavefront: (1) optic axis: the e-ray propagates along a direction whereby its
electric fields (plane of polarization) may oscillate parallel or perpendicular
to the optic axis; (2) speed of light: the speed of o-ray (v⊥) is greater than the speed
of e-ray (v⊥ ³ v ³ v∥) in all directions except along the optic axis of a
positive uniaxial crystal; in other words, v∥ > v⊥ in a negative uniaxial
crystal (See Fig. 2); (3) wavefront: the wavefronts are ellipsoidal
because the speed of e-ray and refractive index vary with angle within the
crystal. Thus, the e-ray does not strictly obey Snell’s law of refraction.
![]() |
Fig. 2 |
“Clearly,
this beam does not follow Snell’s law, but goes in an extraordinary
direction (Feynman et
al., 1963, p. 33–9).”
There were some laughters when Feynman explained
that e-ray does not follow Snell’s law, but it goes in an extraordinary
direction. One may add that the e-ray does not obey Snell’s law even during
normal incidence (q =
0). Furthermore, the e-ray feels a different refractive index
due to the crystal’s anisotropic nature. Some may suggest that Snell’s law still holds for both the o-ray and e-ray,
i.e., the difference being that the refractive index is no longer a constant
for the e-ray. We may justify an extension Snell’s law for the e-ray
by taking into account the anisotropic properties of the crystal. The modified Snell’s Law can have an
effective refractive index that is dependent upon the incident ray, its
polarization, and the relationship with the optical axis (e.g., Lekner, 1991; Wu & Zhang, 2013).
There could be a table to
compare an o-ray and e-ray as shown in the table below. Firstly, the o-ray
obeys Snell’s law, but e-ray does not obey Snell’s law even at normal
incidence. Secondly, the electric fields of o-ray are perpendicular to the
plane containing the incident ray and optic axis, whereas the electric fields
of e-ray are parallel to the plane containing the incident ray and optic axis. Thirdly,
the wavefronts of o-ray are spherical and the wavefronts of e-ray are
ellipsoidal. Fourthly, the refractive index for o-ray is constant no,
but the refractive index for e-ray varies from no to ne depending on the
angle of incidence with respect to the optic axis. Fifthly, the speed of o-ray
in all directions remains constant as v⊥ (c/no), but
the speed of e-ray varies from v⊥ to v∥ (c/ne). The nature of o-ray and e-ray are the same
except the optic axis is oriented differently with respect to the electric
fields of the two perpendicularly polarized light.
|
o-ray |
e-ray |
Snell’s law |
obeys Snell’s law |
does not obey Snell’s law |
Electric fields |
perpendicular to the plane
containing the incident ray and optic axis |
parallel to the plane containing
the incident ray and optic axis |
Wavefronts |
spherical |
ellipsoidal |
Refractive index |
constant no |
varies from no
to ne |
Speed of light |
constant v⊥ (c/no) |
varies from v⊥ to v∥ (c/ne) |
3. Circularly polarized
light:
“We see
therefore that a beam of right circularly polarized light containing a total
energy E carries an angular momentum (with vector directed along the direction
of propagation) E/ω. For when this beam is absorbed that angular momentum
is delivered to the absorber. Left-hand circular light carries angular momentum
of the opposite sign, −E/ω (Feynman et al., 1963, p. 33–10).”
Feynman ended this lecture
by discussing the o-ray and e-ray, but the inclusion of the concept of angular
momentum of circularly polarized light may seem to be a misfit. However, he did
not clarify that the spin angular momentum of a photon may be either +ħ or -ħ in which the signs mean left or right-handedness
respectively (using E = ħω and the convention for ±signs in Optics). Interestingly, photons can have half-integer values of reduced
Planck’s constant (ħ) when they are confined to two dimensions due
to their interactions with one another in certain materials. This is related to
the term anyons for excitations that satisfy any statistics
interpolating bosons and fermions (Wilczek, 1982). The light’s fractional angular momentum can
now be demonstrated experimentally by shining a laser beam through a biaxial
crystal (Ballantine, Donegan, & Eastham,
2016).
Review Questions:
1. How would you define an ordinary ray?
2.
Would you consider an extraordinary ray to be a misnomer?
3. Would you explain that a beam of circularly
polarized light containing a total energy E carries an angular momentum
E/ω that is equal to the reduced Planck’s constant?
The moral of the lesson: an
ordinary ray is a symmetrical (spherical wavefronts) light ray and an
extraordinary ray is an asymmetrical (ellipsoidal wavefronts) light ray because
the optic axis is oriented differently with respect
to the electric fields of the two perpendicularly polarized light.
References:
1. Ballantine, K. E.,
Donegan, J. F., & Eastham, P. R. (2016). There are many ways to spin a
photon: Half-quantization of a total optical angular momentum. Science
Advances, 2(4), e1501748.
2. Feynman, R. P., Leighton, R. B., &
Sands, M. (1963). The Feynman Lectures
on Physics, Vol I: Mainly mechanics, radiation, and heat. Reading,
MA: Addison-Wesley.
3. Lekner, J. (1991).
Reflection and refraction by uniaxial crystals. Journal of Physics:
Condensed Matter, 3(32), 6121.
4. Wilczek, F. (1982). Quantum mechanics of fractional-spin particles. Physical Review Letters, 49(14), 957.
5. Wu, J. F., & Zhang, Y. T. (2013). The relation between the propagation of extraordinary ray and the optical axis in the uniaxial crystal. Optik - International Journal for Light and Electron Optics, 124(17), 2667-2669.
No comments:
Post a Comment