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Aspirin
crystals evaporated from ethol alcohol solution. Copyright
Thomas L. Webster 2004 |
The physics
made very simple... Light rays are composed of waves of light
that vibrate in all planes. When light rays pass through a polarizing
filter only those light rays that are vibrating parallel to the
privileged direction of the polarizing filter are able to
pass through the filter. This results in light rays that are all
vibrating in the same plane of travel. The more oblique the light
rays that strike the front surface of the filter the more these
oblique light rays are filtered out. Perhaps you have noticed
in your own photography that polarizing filters have their greatest
effect on a landscape photograph when the scene being photographed
is oriented 90° to the sun. In this orientation, the polarizing
filter is blocking out the majority of oblique light rays that
contribute to reflections and flare and thereby increases the
saturation of the photograph.
Polarizing
filters come in rotating mounts that allow the photographer to
orient the privileged direction of the polarizing filter to obtain
the highest degree of polarization. If the photographer were to
"stack" two polarizing filters together, view a strong
light source through the stacked filters, and then rotate the
filters, the photographer would see that the light source would
become dimmer and dimmer as the privileged direction of the two
polarizing filters approach 90° in relationship to each other.
Theoretically, when the privileged direction of the two filters
cross at 90°, all light passing through the filters will blocked
(extinguished) and the photographer would no longer be
able to see the light source through the filters. In this orientation,
the polarizing filters are said to be crossed, hence the
term crossed-polarization. In reality, however, due to
the quantum nature of light, a faintly visible and blue-shifted
light source can still be seen. For photographic purposes, though,
the extinction of the light is complete enough.
The splitting
of light into two components (an ordinary light ray and
an extraordinary light ray) by a crystaline substance is
known as birefringence. Birefringence is also known as
"double refraction". Birefringence is the result of
the crystal material having two indices of refraction. One light
ray is slowed down and color shifted compared to another light
ray. Birefringence is caused by the atoms in a crystal having
stronger bonds with one another in one direction and weaker bonds
with one another in a second direction.
If all of
the transmitted light is being extinguished by the crossed-polarizing
filters, then how can a photographer photograph crystals under
the microscope? As regards polarized light, birefringent crystals
come in two "flavors". When struck by strongly polarized
light, isotropic crystals allow transmitted light to pass
through the crystal relatively unaltered. Since the second polarizing
filter is crossed 90° in regards to the first polarizing filter,
a photographer would not be able to view these crystals with crossed-polarizing
filters. Anisotropic crystals, on the other hand, act as
tiny prisms that break up transmitted white light into its constituent
wavelengths of red, blue, green, yellow, and violet light. Uniquely,
anisotropic crystals not only break up white light into its constituent
wavelengths but anisotropic crystals rotate the constituent wavelengths
90° to plane of the polarized light transmitted through the
crystals. The constituent light rays are then able to pass through
the second polarizing filter and expose the film in the camera.
The results are truly kaleidoscopic! (Continue
to Part II...)
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