Physics for Geologists, Second edition
Physics for Geologists, Second edition
Physics for Geologists, Second edition
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52 Optics<br />
Diffraction<br />
If you shine a small light on the edge of an opaque disc above a piece of<br />
paper, the shadow is not sharp. Some light rays passing near the edge are<br />
apparently bent. If you can examine the edge of the shadow, you will find<br />
that it is not just a diffused light, but consists of dark and light bands. This<br />
is diffraction. Diffraction is also the breaking up of light into dark and light<br />
patterns, or colours, when it passes through a grating or discontinuous solid<br />
(such as a crystal) in which the dimensions of the obstacles are not very much<br />
larger than the wavelength of the light.<br />
The theory (due to Fresnel, and later to Huygens) is that each element<br />
of a wave-front acts as a source of vibration itself, sending out secondary<br />
waves. When a wave-front reaches an obstacle, some of these secondary<br />
sources of vibration are destroyed. The remaining sources - some in phase<br />
and so rein<strong>for</strong>cing each other; others out of phase - interfere with each other,<br />
giving the diffraction pattern of alternating light and dark bands. The width<br />
of these bands is proportional to the wavelength, so red light has wider bands<br />
than blue. White light leads to superimposed bands and a spectrum results.<br />
Mother of Pearl owes its colouring to diffraction of ordinary light due to<br />
very fine striations on the shell.<br />
Diffraction gratings<br />
Monochromatic light (i.e. of a single wavelength) passing through a trans-<br />
parent plate with many fine lines ruled onto it takes several paths:<br />
straight ahead, as if there were no lines, and<br />
a scattering of paths, as if the lines were the source of the radiation.<br />
In Figure 4.5, the diffracted ray or beam travels farther than that above<br />
by a distance a = d sin cp, where d is the distance between rays or rulings.<br />
But the beams only rein<strong>for</strong>ce each other when a is an exact multiple of the<br />
wavelength 1. So the grating equation is<br />
nh = d sin cp, (4.5)<br />
where n is an integer and cp is the angle of diffraction. There will also be<br />
a symmetrical pattern diffracted upwards, and there is another solution <strong>for</strong><br />
the supplement of cp, 180 - cp. Note that if d < X, Equation 4.5 can only<br />
have the solution n = 0, that is, cp = 0 or 180". This is not quite what it<br />
seems to be. It is not that all the radiation goes straight through: there is new<br />
radiation going in the same direction, and in the opposite direction.<br />
Polychromatic light (many colours, many wavelengths) will fan out into<br />
spectra on either side of the normal to the grating (Figure 4.6). If we have<br />
a grating with lines at 5 p,m spacing, a first-order radiation of 400 nm (just<br />
visible violet) will be diffracted through 4.59" (n = 1 in Equation 4.5), as<br />
will second-order radiation of 200 nm (n = 2 in Equation 4.5), third-order<br />
Copyright 2002 by Richard E. Chapman