Knyrim K, Vakil N, Pfab R, Classen M
II Medical Klinik, Technische Universität, Munich, Federal Republic of Germany.
Hepatology. 1989 Aug;10(2):134-42. doi: 10.1002/hep.1840100203.
The importance of calcium in gallstone formation is increasingly recognized. Calcium carbonate is an important constituent of gallbladder stones and may be present in the nidus of cholesterol stones. Secondary deposition of calcium carbonate on the surface of cholesterol gallstones is an important reason for failure of oral bile acid dissolution therapy. We sought to determine the effects of bile acids on the crystallization conditions of calcium carbonate in bile. We studied 18 patients with choledocholithiasis with a percutaneous or endoscopically placed catheter high in the biliary tree. Samples of bile in the basal state and following replacement of the bile acid pool with cholic acid, chenodeoxycholic acid and ursodeoxycholic acid were analyzed for total calcium, ionized calcium, bicarbonate and carbonate, and the saturation index for calcium carbonate was calculated. Hepatic bile in the basal state was supersaturated with calcium carbonate. Total calcium concentrations rose linearly with rising bile acid concentrations but ionized calcium was maintained in a relatively narrow range. These data are consistent with an important role for bile acids in binding calcium. Extrapolation of the linear regressions between bile acid concentration and calcium concentrations suggested that in the absence of bile acids, biliary calcium concentrations are in passive equilibrium with plasma. Chenodeoxycholic acid and ursodeoxycholic acid caused a bicarbonate-rich choleresis and significantly augmented the saturation index for calcium carbonate, whereas cholic acid caused no change. In contrast with animal models, the apparent choleretic activity of cholic acid, chenodeoxycholic acid and ursodeoxycholic acid was similar, and no hyper-choleresis was observed with ursodeoxycholic acid. Chenodeoxycholic acid and ursodeoxycholic acid therefore increase the thermodynamic possibility for calcium carbonate precipitation.
钙在胆结石形成中的重要性日益受到认可。碳酸钙是胆囊结石的重要成分,可能存在于胆固醇结石的核心部位。碳酸钙在胆固醇胆结石表面的二次沉积是口服胆汁酸溶解疗法失败的重要原因。我们试图确定胆汁酸对胆汁中碳酸钙结晶条件的影响。我们研究了18例胆总管结石患者,通过经皮或内镜在胆道树高位放置导管。分析基础状态下以及用胆酸、鹅去氧胆酸和熊去氧胆酸替代胆汁酸池后的胆汁样本中的总钙、离子钙、碳酸氢盐和碳酸盐,并计算碳酸钙的饱和指数。基础状态下的肝胆汁中碳酸钙呈过饱和状态。总钙浓度随胆汁酸浓度升高呈线性上升,但离子钙保持在相对较窄的范围内。这些数据与胆汁酸在结合钙方面的重要作用一致。胆汁酸浓度与钙浓度之间线性回归的外推表明,在没有胆汁酸的情况下,胆汁钙浓度与血浆处于被动平衡状态。鹅去氧胆酸和熊去氧胆酸引起富含碳酸氢盐的利胆作用,并显著提高碳酸钙的饱和指数,而胆酸则无变化。与动物模型不同,胆酸、鹅去氧胆酸和熊去氧胆酸的明显利胆活性相似,且未观察到熊去氧胆酸有高利胆作用。因此,鹅去氧胆酸和熊去氧胆酸增加了碳酸钙沉淀的热力学可能性。