Kirks D R
AJR Am J Roentgenol. 1979 Sep;133(3):383-8. doi: 10.2214/ajr.133.3.383.
Bile salts are formed from cholesterol and conjugated in the liver, excreted via the biliary system into the duodenum, reabsorbed in the ileum, stored temporarily in the hepatic bile salt pool, and reexcreted into the biliary system. This normal enterohepatic circulation of bile salts is both efficient and rapid. Interruption of the enterohepatic circulation of bile salts may cause cholesterol cholelithiasis or oxalate urolithiasis. Clinical and radiologic features of pediatric patients with gallstones and urolithiasis secondary to abnormalities of the ileum are reported. The pathophysiology of lithiasis due to interruption of the enterohepatic circulation of bile salts is discussed. This enteric cause is included in the differential diagnosis of cholelithiasis and urolithiasis in infants and children.
胆盐由胆固醇形成并在肝脏中结合,经胆道系统排入十二指肠,在回肠重吸收,暂时储存于肝内胆盐池,然后再排入胆道系统。这种正常的胆盐肠肝循环高效且迅速。胆盐肠肝循环中断可能导致胆固醇性胆结石或草酸钙性尿路结石。本文报道了因回肠异常继发胆结石和尿路结石的儿科患者的临床及影像学特征。讨论了胆盐肠肝循环中断导致结石形成的病理生理学。这种肠道病因被纳入婴幼儿胆结石和尿路结石的鉴别诊断中。