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胆结石成因与地球化学环境关系的探索
引用本文:夏亮芳,胡韵.胆结石成因与地球化学环境关系的探索[J].贵阳医学院学报,1990,15(4):281-285.
作者姓名:夏亮芳  胡韵
作者单位:贵阳医学院外科学教研室,贵阳医学院外科学教研室,贵阳医学院外科学教研室,中国科学院地球化学研究所,中国科学院地球化学研究所,中国科学院地球化学研究所,从江县人民医院,从江县人民医院
摘    要:贵州省贵阳市以胆固醇结石为主的胆囊结石占77.56%,而从江县以胆色素结石为主的原发性肝胆管结石占66.89%。作者取贵阳市和从江县两地区胆石进行成份分析、水质分析、土壤微量元素分析,并比较两地区地理、地貌、地层、岩性、气候和生活习性差异,以探索胆结石成因与地球化学环境的关系。初步发现胆固醇结石多发于碱性硬水地区,而胆色素结石多发于酸性软水地区。

关 键 词:胆结石  病因  碱性硬水  胆固醇结石

The Relationship Between the Regional Environment and the Genesis of Gallstones
Xia Liangfang,et al.The Relationship Between the Regional Environment and the Genesis of Gallstones[J].Journal of Guiyang Medical College,1990,15(4):281-285.
Authors:Xia Liangfang  
Institution:Xia Liangfang,et al Department of Surgery
Abstract:The relationship between regional environment and gallstone genesis of Guiyang City and Chongjiang County has been studied.The geologic, geographic and climatic situation between those of two places are different :Guiyang City is located in the alpine basin of middle Guizhou covered by limestone with a temperate climate, on the contrary, Chongjiang County in the south-east of Yunnan-Guizhou plateau covered by slate with a subtrop- ical mild-humid climate.The differences are also shown in gallstone types, there are 77.56% cholesterol stones in Guiyang, while 68.89% pigmental stones in Chongjiang.The contents of K, Na, Ca, Mg, Mn, Cl, Fe, Cu, Co, Al and P stones in Chongjiang are higher than those in Guiyang.As a drinking water acidic soft water, pH=6.03, rich in Na~+, K~+ and Cl~-for the Chongjiang and alkali hard water pH=7.9, rich in Ca~(2+), Mg~(2+), dissolved gas O_2, HCO_3~-, SO_4~(2-) and plasma NH_4NO_2~-, NO_3~-is typical for the Guiyang, The contents of Pb, Ni and Cr of soil the Guiyang are 21, 18, 84 times greater tnan tnose in the Chongjiang respectively.From above described, a preliminary conclusion can be gotten, that cholesterol gallstone mostly formed in alkali hard water area, and pigmental gallstone in acidic soft water area.
Keywords:cholesterol stone  alkali hard water  pigmental stone  acidic soft water
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