T. Murayama et al., Role of the diurnal variation of urinary pH and urinary calcium in urolithiasis: A study in outpatients, INT J UROL, 8(10), 2001, pp. 525-531
Background: We previously reported that the urinary excretion of calcium an
d the diurnal variation of urinary pH were important for stone formation in
hospitalized inpatients with hospital standard diet. Because almost all ur
inary stones are formed in outpatients with ambulatory free diet, it is ess
ential to investigate these factors in outpatients.
Methods: We examined the urinary excretion of calcium, oxalate, uric acid,
phosphate and magnesium in 96 male outpatients and 142 male inpatients. We
also studied the relationship between the stone composition and the diurnal
variation of urinary pH in 32 male outpatients (five uric acid stones (UA)
, 13 pure calcium oxalate stones (CaOX) and 14 mixed calcium oxalate and ca
lcium phosphate stones (CaOX-CaP)) and 53 male inpatients (nine UA, 15 CaOX
and 29 CaOX-CaP).
Results: There was a significant difference in the urinary excretion of cal
cium among outpatients with UA, CaOX and CaOX-CaP (133 +/- 96 vs 219 +/- 97
vs 268 +/- 102 mg per day, P < 0.05). In outpatients with UA, urinary pH w
as constantly low throughout the entire day. In contrast, outpatients with
CaOX and those with CaOX-CaP had diurnal variation of urinary pH that was l
ow in the early morning, followed by elevation in the daytime and was lower
ed in the night. The pHs in the early morning, afternoon and night were sig
nificantly higher in outpatients with CaOX-CaP than in those with CaOX.
Conclusion: The diurnal variation of urinary pH and the urinary calcium are
important for stone formation.