V. Pichette et al., AMMONIUM ACID URATE CRYSTAL-FORMATION IN ADULT NORTH-AMERICAN STONE-FORMERS, American journal of kidney diseases, 30(2), 1997, pp. 237-242
Although ammonium acid urate (AAU) stones are endemic in Asia, pure AA
U calculi have almost disappeared from industrialized countries and cl
inical pathophysiologic relevance of sporadic stones containing AAU cr
ystals is currently unknown, We reviewed 1,396 crystallographic stone
analyses performed in our institution over a 10-year period, Prevalenc
e of stones containing AAU crystals and predominantly AAU stones were
3.1% and 0.2%, respectively, In more than two thirds of cases, AAU cry
stals represented less than 10% of stone crystal composition, No pure
AAU stone was found, According to crystalline predominance, 42%, 35%,
and 12% of these calculi were uric acid, infectious, and calcium oxala
te stones, respectively, AAU crystals were detected as discrete interc
rystalline or peripheral deposits in 74.4% of stones. In only one calc
ulus was AAU crystals detected in the nucleus, The hospital charts of
37 patients who presented with 43 calculi containing AAU crystals were
also reviewed, The mean age was 53.1 +/- 16.6 years, Fifty-seven perc
ent of calculi were upper urinary tract stones and 43% were bladder st
ones, Upper urinary tract calculi were more frequently uric acid stone
s, followed by infectious and calcium oxalate stones. Lower urinary tr
act calculi were more frequently infectious stones, followed by uric a
cid stones, Upper urinary tract stones were passed spontaneously in 13
patients and removed surgically in nine patients, Nine of these subje
cts were idiopathic recurrent stone formers who had passed other calcu
li with no trace of AAU crystal, Fifty-seven percent of lower urinary
tract stones were associated with documented bladder dysfunction. In c
onclusion, although AAU-containing urolithiases are occasionally seen
in our population, predominantly or primarily AAU stones are exception
al. AAU crystal formation usually appears as a minor and secondary phe
nomenon of no primary pathophysiologic relevance in stone formation. (
C) 1997 by the National Kidney Foundation, Inc.