 Solution

Randomly oriented crystallites supply planes with their normals in each required scattering-vector direction. Of the five families considered, $(111)$, $(200)$ and $(220)$ can therefore give accessible copper $K_{\alpha }$ powder peaks; $(300)$ remains absent and $(640)$ remains beyond a roughly $130^{\circ }$ detector limit. Other allowed families also appear if their Bragg angles lie inside the instrument range; orientation averaging does not restrict the pattern to these five examples.

Only a small fraction of randomly oriented crystal grains satisfy the Bragg condition for a given detector setting, and each family scatters around a cone rather than concentrating all its intensity into one single-crystal spot. A narrow detector aperture therefore receives a relatively weak signal from a small powder specimen compared with a well-oriented large single crystal. Adequate crystal grain statistics, longer counting, suitable powder packing and detector acceptance matter. The odd-parity peaks additionally involve the difference of ionic scattering factors. No absolute single-crystal/powder intensity ratio follows without illuminated volumes, absorption and instrumental geometry.