The beryllium lattice has a low solubility for most of the elements, C
ritical enrichments may lead to precipitation and consequently to the
formation of stable subgrain boundaries. Therefore, it is important to
characterize the local impurity concentrations in beryllium single cr
ystals. By the Rutherford back-scattering technique, the local chemica
l composition can be examined to a high degree of sensitivity. Within
a subgrain boundary, strong local enrichments of iron and oxygen were
determined, A periodical accumulation of iron and carbon was found in
the growth direction of the beryllium single crystals. It is suggested
that constitutional supercooling effects control the local formation
of the precipitations in the crystals.