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ChromotherapyScience
of Light
Lesson Six |
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Lesson
six, page 2
In 1800 W. Herschel studied heat distribution with
the aid of thermometers and found the maximum temperature
beyond the red end of the spectrum, thus discovering the
infrared spectrum. Then
in 1801 J.W. Ritter, in studying the effect of spectral
light on silver salts, found this action extending beyond
the violet and thus discovered the ultraviolet spectrum.
The next year Thomas Young established the first
connection between the wave-length theory and the
spectrum; and he calculated the approximate wave lengths
of the colors recognized by
Throughout the 19th century further
discoveries were made by famous scientists in measuring
the solar spectrum, and comparing this with the spectrum
of flames, or the sparks of pure elements.
In 1868 A.J. Angstrom established and loaned his
name to a new unit of wave-length measurement, the
angstrom, which in spectroscopy is one ten-millionth part
of a millimeter, or one ten-billionth of a meter.
Another method of studying the spectrum is by use
of a grating; ruling fine parallel lines with a diamond
point on glass or copper, then studying the rays, which
are diffracted in this case.
The advantage of this method lies in the
possibility of studying not only the visible spectrum, but
also the ultraviolet and infrared spectra as well.
There are generally four ways of observing spectra: that is, visually, photoelectrically, radiometrically, and photographically. Each is useful in a different way. Although the average human eye is most sensitive to green light (5500 angstroms), its sensitivity declines rapidly to zero for infrared (7700 A), and ultraviolet (3800 A).
Visual methods of observation are of little value
in the study of spectroscopy.
Eyesight is too selective, variable and restricted
to one octave. Therefore
extensive instruments have been devised to eliminate error
in judgment. These
have become so refined that the presence of helium was
detected on the sun in 1868, a generation before it was
shown to be present on earth.
Spectroscopic measurements are concerned
essentially with energy distribution as a function of
wavelength. The
visible spectrum ranges from about 3800A (violet limit) to
7700A (red limit). Extremely
short waves, such as those in the x-ray range are only
about 0.1A to about 100A, and therefore a different, more
practical unit of measurement is used for x-ray, called
the x unit, and still another for the extremely long
infrared heat waves, which are measured in larger units
called microns.
Some instruments used to measure
light:
A
spectrometer
is an instrument used to determine the index of refraction
by measuring the external angle of a prism, and its angle
of minimum deviation.
(Also classified among spectroscopes)
A
spectroscope
is any of various instruments designed for forming and
examining optical spectra, constructed to enable one to
make observations visually.
Lesson
six, page 3
A
spectrograph
is used to photograph the spectrum.
A
spectrophotometer
is a photometer for measuring the relative intensities of
light in different parts of a spectrum, or the relative
intensity of two spectra.
A
photometer
is any instrument for measuring the intensity of light, or
comparing the relative intensity of several lights.
Color is a response of the human observer to
visible light energy, which is a small part of the total
electromagnetic spectrum.
An object is visible because it is able to reflect
light, for color is not in an object but in the reactions
of the eye to the vibration of the object.
There are at least six things that work together to
produce the color we see.
They are the light source, the light itself, the
material medium through which the light travels, the
object on which the light falls, the eye, and the brain.
When we see the color of an object, it is the last
step in a chain of events that begins at a light source.
The light source generally sends out a mixture of
light rays of many wave lengths.
As the rays pass through the air to the object, the
air attenuates some of the light of short wave-length by
scattering it. When
the light falls on the object, the object removes some
more light by absorbing it.
What is left of the light is then reflected or
transmitted from the object through the air to our eyes.
Once again the air removes some light.
The color we see depends on the kind of light
mixture that finally reaches our eyes.
But it depends, too, on the nature of our eyes, and
the message that our eyes send to the brain.
When the light of one color and wave length falls
on an object, the object divides the light into three
parts. One
part of the light is allowed to pass right through, as if
the object were full of holes and the light went through
the holes. We
say that this part of the light has been transmitted.
Another part
of the light bounces back from the object, the way a ball
bounces back from a wall.
We say that this part of the light has been
reflected. A
third part of the light is trapped in the object and is
not allowed to escape.
Usually the trapped light is turned into heat.
We say that this part of the light has been
absorbed.
While white objects reflect back all colors, and
black reflect none, there are some things that reflect
only part of the light that shines on them, and treat all
colors impartially. These
objects appear gray, because gray is an “impartial
reflector”.
Lesson
six, page 4
A gray object may look white when it is the
brightest thing of all that can be seen at the same time.
It looks black when it is the least bright of all
things visible. But
it looks gray when there are both brighter and less bright
objects within view. So
whether an object looks white or black or gray depends not
only on the light that it sends to your eyes, but also on
a comparison between this light and the light sent by
other objects. This
comparison is made by your brain, unconsciously.
The dictionary defines color as “a visual
attribute of bodies or substances, distinct from their
characteristics of size, form or texture.
The appearance of color depends upon the spectral
composition of wavelengths of radiant energy capable of
stimulating the retina and its associated neural
structures”.
The separation of colors in the spectrum is due to
the fact that different colors have different wave
lengths. Practical
limits of the visible wave lengths are about 16 millionths
and 28 millionths of an inch.
Each different wave length produces in the eye the
sensation of a different color.
The given wave length associated with each color of
the visible spectrum is as follows:
Color
Wavelength
Violet
17 millionths of 1 inch
Indigo
18 millionths of 1 inch
Blue
19 millionths of 1 inch
Green
20 millionths of 1 inch
Yellow
23 millionths of 1 inch
Orange
24 millionths of 1 inch
Red
27 millionths of 1 inch
Precious stones such as diamonds flash colored
light that is very beautiful. These transparent stones are
formed of materials that slow down light waves very
markedly. In a
pure diamond, made only of carbon atoms, light travels
scarcely half as fast as it does in air.
The gems are cut and polished to have dozens of small
surfaces, called facets, so that many little prisms are
formed. Light
that shines into such a cut stone is refracted in many
directions. The
“fire” of a good diamond comes from the breaking up of
white light into many colors by its tiny prisms.
The greater the index of reflection, the greater the
extent to which a light beam is deflected upon entering or
leaving that medium. Diamonds
owe their brilliance to that very high index of refraction.