Page 14 - Modern physical chemistry
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1.3 Diffraction

                In the simple diffraction setup of figure  1.2, monochromatic (sinusoidal) radiation
             strikes a plane containing equispaced parallel scattering lines at angle 0 and is observed
             at angle ¢J  above the plane. Maxima in the radiation are found at certain angles, which
             we number, taking 0 as the order when ¢J equals 0, 1 as the order for the first larger angle,
             2 for the second larger one, and so on.
                Each maximum occurs where neighboring rays reinforce each other as much as pos-
             sible. That is, where a crest of one ray reaches the observer at the same time as a crest
             of each of its neighbors, a trough at the same time as a trough of each of its neighbors.
             But at other angles, the diffracted ray labeled 2 cancels part of the one labeled 1, and so
             on. Thus, the intensity drops very fast on each side of a maximum.
                Since the rays labeled 1 and 2 start in phase at their source, they are reflected in phase,
             with the crests matching at the observation point, when the extra path length along 1 equals
             an integral number of wavelengths. But from figure  1.2, this extra length equals the pro-
             jection of the distance between scattering lines on the incident ray 1 minus its projection
             on the reflected ray 2:
                                           nA = d(cosO -COS41).                       [1.1]


                Note that n is the order of the reflection, A the wavelength of the radiation, d the dis-
             tance between lines, 0 the glancing angle at which the rays strike the grating, and ¢J  the
             angle at which the diffracted rays leave the grating.
                A person can detennine d  directly by counting the number of lines per millimeter
             under a microscope, or indirectly by measuring how radiation of known wavelength is
             diffracted. With the short wavelength radiation needed to study crystals and with avail-
             able gratings, angles 0 and ¢J  are quite small. Nevertheless, they can be very accurately
             measured, so A can be found to about six significant figures.

             Example 1.1

                X rays of wavelength 0.710 A strike a grating at a glancing angle 0 equal to 5' 0". If the
             grating contains 200 lines cm- evenly spaced, at what angle ¢J  would the first-order dif-
                                       1
             fraction peak be found?
                This diffraction is governed by formula (Ll) with

                                 n=l,    A = 0.710 x 10- 8  cm,   d=   1   ,
                                                               200 cm- 1

                                    (5minX3.1416 radians)
                                 0=                     = 0.001454 radians.
                                    (  60 min deg- ¥ 180deg)
                                               1
             Because the angles are small, higher terms in the expansions
                                                     0 2
                                           cosO = 1 - -  +  ... ,
                                                      2
                                                     41 2
                                            cos41 = 1 - -  +  ... ,
                                                      2
             which are valid when the angles are in radians, can be neglected.
                Then
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