Bl. Auer et al., THE EFFECT OF ASCORBIC-ACID INGESTION ON THE BIOCHEMICAL AND PHYSICOCHEMICAL RISK-FACTORS ASSOCIATED WITH CALCIUM-OXALATE KIDNEY-STONE FORMATION, CLINICAL CHEMISTRY AND LABORATORY MEDICINE, 36(3), 1998, pp. 143-147
The present study was undertaken to determine the effect of ingestion
of large doses of vitamin C on urinary oxalate excretion and on a numb
er of other biochemical and physicochemical risk factors associated wi
th calcium oxalate urolithiasis. A further objective was to determine
urinary ascorbate excretion and to relate it qualitatively to ingested
levels of the vitamin and oxalate excretion. Ten healthy males partic
ipated in a protocol in which 4 g ascorbic acid was ingested for 5 day
s. Urines (24 h) were collected prior to, during and after the protoco
l. The urine collection procedure was designed to allow for the analys
is of oxalate in the presence and absence of an EDTA preservative and
for the analysis of ascorbic acid by manual titration using 2,6 dichlo
rophenolindophenol. Physicochemical risk factors such as the calcium o
xalate relative supersaturation and Tiselius risk index were calculate
d from urine composition. The results showed that erroneously high ana
lytical oxalate levels occur in the asence of preservative. In the pre
served samples there was no significant increase in oxalate excretion
at any stage of the protocol. Ascorbate excretion increased when vitam
in C ingestion commenced but levelled out after 24 hours suggesting th
at saturation of the metabolic pool is reached within 24 hours after w
hich ingested ascorbic acid is excreted unmetabolized in the urine. Wh
ile transient statistically significant changes occurred in some of th
e biochemical risk factors, they were not regarded as being clinically
significant. There were no changes in either the calcium oxalate rela
tive supersaturation or Tiselius risk index. It is concluded that inge
stion of large doses of ascorbic acid does not affect the principal ri
sk factors associated with calcium oxalate kidney stone formation.