Purpose: We evaluated the role of mucus in urine after bladder augment
ation and hypothesize that mucus acts as a possible etiological factor
in stone formation. Materials and Methods: Mucus was collected via ce
ntrifugation from the 24-hour urine specimens of 8 stone forming and 1
0 nonstone forming patients who were randomly selected from our augmen
tation population. The mucus and stones were lyophilized, and then ana
lyzed via scanning electron microscopy and energy dispersive x-ray spe
ctrometry for calcium, phosphate, magnesium and sodium. The 24-hour ur
ine collections were also analyzed to determine any metabolic differen
ces between the 2 groups. Results: Scanning electron microscopy and en
ergy dispersive x-ray spectrometry spectra showed increased calcium, p
hosphate, and magnesium, and significantly higher (p <0.05) calcium-to
-phosphate ratios in the mucus of stone versus nonstone forming patien
ts. Of the 8 stones examined all had viscous fluid (mucus) centers ric
h in calcium, phosphate and magnesium. Calcium-to-phosphate ratios in
the corresponding mucus recovered from stone centers were similarly hi
gh. Urinary citrate levels were low in both groups, and calcium, phosp
hate and magnesium were within normal ranges. Conclusions: Mucus appea
rs to have an important role in the genesis of bladder stones after au
gmentation, possibly acting as a nidus. Metabolic changes following au
gmentation were similar in stone and nonstone forming populations. Our
data suggest that mucous calcium-to-phosphate ratios may be predictiv
e of future stone formation. Furthermore, there may be a benefit in in
stituting more aggressive measures aimed at clearing mucus from the bl
adder.