A simple modification to the fast T-1 translation function of Crowther
& Blow [Crowther & Blow (1967). Acta Cryst. 23, 544-548] can reduce s
ystematic error in cases where the input set of oriented search models
represents a fraction of the scattering matter of the unknown crystal
unit cell. The observed Patterson function is modified by a partial s
elf-vector subtraction (SVS) and then the residual Patterson origin is
removed In a test case where a protein/DNA complex crystal was search
ed using a protein-only model, the highest signal-to-noise ratios for
translation-search maps were obtained either with origin removal alone
or partial SVS combined with origin removal. Origin removal is likely
to be a generally useful alternative to SVS for the T-1 function.