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Diploma Thesis - Erich Schmid Institute

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Basic X-ray diffraction<br />

Equation 3.9 is valid for all crystal systems, and the components of G can be<br />

replaced by the points of intersection u1, u2 and u3 of the net plane with the elongated<br />

translation vectors a1, a2 and a3.<br />

Figure 3.1: Crystallographic plane and surface normal<br />

The components of G are for that reason:<br />

1<br />

h =<br />

u1<br />

1<br />

k =<br />

u2<br />

1<br />

l = (equ. 3.10)<br />

u<br />

3<br />

5

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