A brief calculation is made to estimate the amount of secondary extinc
tion in polycrystals with no preferred orientations. To this end, use
has been made of the Zachariasen's general theory of X-ray diffraction
in crystals, together with corrections introduced by Cooper and Rouse
. It was found, that secondary extinction is negligible, so that any e
xtinction observed is primary in origin, which is related to the dislo
cation density.