The composition of urinary stones in children depends on socioeconomic cond
itions and hygiene, geographical area, and dietary habits. We analyzed urin
ary stones from 120 consecutive Tunisian children (81 males, 39 females) ag
ed 5 months to 15 years. The stone was located in the upper urinary tract i
n 91 cases (76%). Stone analysis included both a morphological examination
and an infrared analysis of the nucleus and the inner and peripheral layers
. The main components of bladder calculi were whewellite (69%) and struvite
(22%), whereas the main component of upper urinary tract calculi was whewe
llite (67%). The nucleus of bladder stones was composed of ammonium urate (
45%), struvite (28%), cystine (10%), and carbapatite (7%), The nucleus of k
idney and ureteral calculi was mainly composed of ammonium urate (38%), whe
wellite (24%), carbapatite (13%), or struvite (11%). Based on stone composi
tion, urinary tract infection was involved in the nucleation or growth of a
third of calculi. Endemic urolithiasis involving simultaneous nutritional,
metabolic, and infectious factors, and defined by its nucleus composed of
ammonium urate without struvite, represented 40% of cases. Exclusive metabo
lic factors - including genetic diseases such as primary hyperoxaluria, cys
tinuria, and hypercalciuria - were responsible for less than 25% of cases.