Role of the diurnal variation of urinary pH and urinary calcium in urolithiasis: A study in outpatients

Citation
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
Citations number
17
Categorie Soggetti
Urology & Nephrology
Journal title
INTERNATIONAL JOURNAL OF UROLOGY
ISSN journal
09198172 → ACNP
Volume
8
Issue
10
Year of publication
2001
Pages
525 - 531
Database
ISI
SICI code
0919-8172(200110)8:10<525:ROTDVO>2.0.ZU;2-B
Abstract
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.