Physics for Geologists, Second edition
Physics for Geologists, Second edition
Physics for Geologists, Second edition
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Optics 53<br />
Figure 4.5 Diffraction of monochromatic light through a grating. There is<br />
a symmetrical set of beams diffracted upwards.<br />
Figure 4.6 Diffraction of polychromatic light through a grating (diagrammatic).<br />
radiation of 133 nm, fourth-order radiation of 100 nm, and so on. At the<br />
other end of the visible spectrum, radiation of 750nm will be diffracted<br />
through 8.63", as will 375 nm, 250 nm, etc.<br />
This overlap of wavelengths does not lead to practical difficulty. If the<br />
observation is visual, all the radiation of second-order and above is outside<br />
the visible spectrum. If the observation is photographic, emulsions can be<br />
chosen to detect specific ranges of wavelength (within limits).<br />
Rainbows<br />
Be<strong>for</strong>e leaving the subject of reflection and refraction, consider as a digres-<br />
sion of general interest, the common rainbow. It is caused by refraction<br />
and internal reflection of sunlight falling on a raindrop (or spray from<br />
a waterfall). Why is the sun low in the sky when there is a rainbow?<br />
Why do you never see a completed circle of rainbow unless you are in an<br />
Copyright 2002 by Richard E. Chapman