The possible effects of Zn and Cu in oxalocalcic urolithiasis were inv
estigated. The formation of calcium oxalate crystals in the presence o
f Zn and Cu demonstrated that their morpholoy is clearly affected by t
hese ions. Thus, when such ions were present in a number of higher con
centrations, a notable increase in the primary aggregation was clearly
detected. On the other hand, Zn and Cu urinary levels were determined
in groups of stone-formers and healthy people. Zinc urinary concentra
tion was significantly lower for lithiasic than for healthy people and
the copper urinary concentration was lower for lithiasic than healthy
males, but both female groups had a similar copper urinary concentrat
ion. The mentioned differences disappeared when serum levels were cons
idered. These obtained results have been comparatively evaluated with
those obtained by other authors. When considering all the commented as
pects, it is concluded that no important direct action of zinc and cop
per on oxalocalcic calculi genesis takes place.