论文部分内容阅读
对50例肝内结石及100例肝胆管结石病组织进行结构及组化观察,发现胆石基质存在致密层及疏松层结构,两者粘液分布不同,致密层以中性粘液为主,并呈树枝状伸入疏松层,显示其层间联接作用。胆石疏密结构的形成可能与胆管炎症周期胆管内环境变化有关。胆石基质主要含硫酸性及中性粘液,后者主要来自肝胆管增生的壁内腺。这表明中性粘液的出现与胆石形成有密切关系。
Fifty cases of intrahepatic stones and 100 cases of hepatolithiasis were observed by microstructure and histology. The results showed that there was a dense layer and a loose layer in the gallstone matrix. The distribution of mucus in the two layers was different. The dense layer was mainly composed of neutral mucus, Shape into the loose layer, showing the role of the interlayer connection. The formation of gallstone sparse structure may be related to the bile duct inflammation cycle bile duct environment. Gallstone matrix contains mainly sulfuric acid and neutral mucus, the latter mainly from the wall of the gland bile duct proliferation. This shows that the emergence of neutral mucus and gallstone formation are closely related.