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Urolithiasis in Tunisian children: a study of 100 cases
Akram Alaya1, Abdellatif Nouri, Mohamed Fadhel Najjar
1Department of Biochemistry and Toxicology, University Hospital, Monastir, Tunisia. akram_alaya@yahoo.co.uk
Insights
Pediatric urolithiasis in Tunisia shows a shift towards calcium oxalate stones, primarily in the upper urinary tract. While males are still more affected, the gender disparity in childhood kidney stones is decreasing.
Area of Science:
- Pediatric Nephrology
- Urology
- Clinical Chemistry
Background:
- Renal stone disease in children presents unique challenges.
- Understanding the epidemiological and etiological profiles of pediatric urolithiasis is crucial for effective management.
Purpose of the Study:
- To investigate the clinical and biological characteristics of kidney stone disease in children from Tunisia's coastal region.
- To identify trends in the composition and location of urinary stones in pediatric patients.
Main Methods:
- A retrospective, multi-center study involving 100 children under 16 with urinary stones.
- Review of patient charts for demographics, clinical presentation, and laboratory/radiological findings.
- Infrared spectrophotometry for stone analysis.
Main Results:
- The male to female ratio was 1.5:1, with dysuria being the most common symptom.
- Upper urinary tract stones occurred in 76% of cases; 13% had positive urine cultures.
- Whewellite (calcium oxalate) was the predominant stone type (77%), often found in the upper tract, while struvite stones were more common in the lower tract.
Conclusions:
- The epidemiological profile of pediatric renal stones in Tunisia is evolving, with a rise in calcium oxalate stones and upper tract involvement.
- The traditional male predominance in pediatric urolithiasis appears to be diminishing in the region.
Abstract:
The aim of this study is to assess the clinical and biological characteristics of renal stone disease among children living in the coastal region of Tunisia. This retrospective multi-center study included 100 children under the age of 16 years, who presented with urinary stones. The patients' charts were reviewed with regard to age at diagnosis, sex, history and physical examination as well as laboratory and radiologic findings. Stone analysis was performed by infrared spectrophotometry. The male/female sex ratio was 1.5 to 1. The clinical presentation of this pathology was dominated by dysuria. Stones were located in the upper urinary tract in 76 cases (76%). A total of 13% of the study subjects had positive urine cultures. Metabolic investigations were performed in all patients and were normal in 80 cases. Whewellite (calcium oxalate) was found in 77 stones (77.0%). Stone section was made of whewellite in 69.0% of cases and ammonium urate in 47.0%. Struvite stones were more frequently seen in the lower urinary tract. Our study suggests that the epidemiological profile of renal stones in Tunisia has changed towards a predominance of calcium oxalate stones and upper tract location. Also, the male predominance of pediatric urolithiasis is becoming less obvious in Tunisia.
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