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Alterations in bile following urinary intestinal diversion.
1Department of Urology, Vanderbilt University Medical Center, Nashville, Tennessee.
The Journal of Urology
|October 1, 1992
Summary
Urinary diversion using intestinal segments did not significantly alter bile composition or increase its tendency to form stones (lithogenicity). This finding aligns with the absence of gallstones in children undergoing similar urinary intestinal diversion procedures.
Area of Science:
- Gastroenterology
- Urology
- Biliary Physiology
Background:
- Urinary intestinal diversion involves rerouting urine through a segment of the bowel.
- Potential alterations in bile composition and lithogenicity following such procedures are not fully understood.
- Cholelithiasis (gallstone formation) is a clinical concern in patients with urinary intestinal diversion.
Purpose of the Study:
- To investigate if intestinal segments used in urinary diversion alter bile composition.
- To determine if these alterations increase bile lithogenicity.
- To correlate findings with clinical observations of gallstone formation in pediatric patients.
Main Methods:
- 42 female Sprague-Dawley rats underwent intestinal and urointestinal manipulations.
- Timed bile collections were obtained from the common bile duct.
- Bile was analyzed for acids, phospholipids, cholesterol, bilirubin, volume, osmolality, pH, and electrolytes (calcium, chloride, sodium, potassium).
Main Results:
- Specific changes in bile constituents were observed based on the type of urinary diversion and bowel segment used.
- These identified changes were not significant enough to alter bile lithogenicity.
- No substantial increase in the risk of gallstone formation was detected in the experimental model.
Conclusions:
- Urinary diversion with intestinal segments does not render bile significantly more lithogenic.
- Experimental findings support the clinical observation of a lack of cholelithiasis in children with urinary intestinal diversion.
- Bile composition changes are specific but do not reach a threshold for pathological lithogenesis.