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青木关地下河中溶解态甾醇来源及迁移、转化特征
引用本文:梁作兵,沈立成,孙玉川,王尊波,江泽利,张媚,廖昱,谢正兰,张远瞩.青木关地下河中溶解态甾醇来源及迁移、转化特征[J].环境科学,2015,36(11):4074-4080.
作者姓名:梁作兵  沈立成  孙玉川  王尊波  江泽利  张媚  廖昱  谢正兰  张远瞩
作者单位:西南大学地理科学学院, 三峡库区生态环境教育部重点实验室, 重庆 400715;西南大学地理科学学院, 三峡库区生态环境教育部重点实验室, 重庆 400715;中国地质科学院岩溶地质研究所, 国土资源部岩溶动力学重点实验室, 桂林 541004;西南大学地理科学学院, 三峡库区生态环境教育部重点实验室, 重庆 400715;中国地质科学院岩溶地质研究所, 国土资源部岩溶动力学重点实验室, 桂林 541004;西南大学地理科学学院, 三峡库区生态环境教育部重点实验室, 重庆 400715;西南大学地理科学学院, 三峡库区生态环境教育部重点实验室, 重庆 400715;西南大学地理科学学院, 三峡库区生态环境教育部重点实验室, 重庆 400715;西南大学地理科学学院, 三峡库区生态环境教育部重点实验室, 重庆 400715;西南大学地理科学学院, 三峡库区生态环境教育部重点实验室, 重庆 400715;西南大学地理科学学院, 三峡库区生态环境教育部重点实验室, 重庆 400715;中国地质科学院岩溶地质研究所, 国土资源部岩溶动力学重点实验室, 桂林 541004
基金项目:中央高校基本科研业务费专项(XDJK2013B021,XDJK2015D003); 西南大学博士基金项目(SWU110258); 应对全球气候变化地质调查综合研究项目(12120113006700); 重庆市科委院士专项(cstc2013jcyjys20001); 岩溶动力学重点实验室开放基金项目(KDL2011-04,KDL201303); 重庆市研究生科研创新项目(CYS14056)
摘    要:为阐述溶解态甾醇在地下河中的来源及迁移、转化过程和对水质状况评价,2013年7~11月在青木关地下河入口处、出露处和出口处进行定期采样,并利用气相色谱-质谱联用仪(GC-MS)对样品中溶解态甾醇的组分进行定量分析.结果表明,7~11月溶解态甾醇的平均含量变化为415~629 ng·L-1,随月份的增加地下河中溶解态甾醇的含量呈下降的趋势;从地下河入口至地下河出口溶解态甾醇的平均含量变化为724~374 ng·L-1;豆甾醇/胆固醇的平均比值变化为0.29~0.12,随地下河运移距离的增加二者的值均呈下降的趋势.成分组成上以胆固醇含量占优势,约占总含量的37.30%~94.85%,但各月组成变化较大.粪醇/胆固醇、粪醇/甾醇总量的比值均小于0.2,表明没有受到生活污水的污染,但随月份的增加二者比值大致呈增加的趋势.

关 键 词:土壤固碳  溶解性有机质  生物标志物  甾醇  青木关地下河
收稿时间:4/4/2015 12:00:00 AM
修稿时间:6/9/2015 12:00:00 AM

Sources, Migration and Conversion of Dissolved Sterols in Qingmuguan Underground River
LIANG Zuo-bing,SHEN Li-cheng,SUN Yu-chuan,WANG Zun-bo,JIANG Ze-li,ZHANG Mei,LIAO Yu,XIE Zheng-lan and ZHANG Yuan-zhu.Sources, Migration and Conversion of Dissolved Sterols in Qingmuguan Underground River[J].Chinese Journal of Environmental Science,2015,36(11):4074-4080.
Authors:LIANG Zuo-bing  SHEN Li-cheng  SUN Yu-chuan  WANG Zun-bo  JIANG Ze-li  ZHANG Mei  LIAO Yu  XIE Zheng-lan and ZHANG Yuan-zhu
Institution:Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China;Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China;Key Laboratory of Karst Dynamics, Ministry of Land and Resources, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China;Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China;Key Laboratory of Karst Dynamics, Ministry of Land and Resources, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China;Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China;Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China;Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China;Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China;Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China;Key Laboratory of the Three Gorges Reservoir Region's Eco-Environment, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China;Key Laboratory of Karst Dynamics, Ministry of Land and Resources, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China
Abstract:Water samples were collected from the Qinmuguan underground river from July to November in 2013. By gas chromatography-mass spectrometer (GC-MS), dissolved sterols were quantitatively analyzed. The results show that the average variation content of dissolved sterols ranges from 415 to 629ng ·L-1, with the increasing migration distance of dissolved sterols in underground river, its contents are decreased. Between the inlet and outlet of Qingmuguan underground river, the average variation contents of dissolved sterol are between 724 and 374ng ·L-1, and the average variation ratios of the content of stigmasterol with cholesterol range from 0.29 to 0.12. In short,their values are decreased accompanied by the increasing migration distance of underground river. The composing component in dissolved sterols varied differently between July to December, and the main component of dissolved sterols is cholesterin, the ratios of the content of dissolved sterols with cholesterin to the total dissolved sterols range from 37.30% to 94.85%. In addition, the ratios of the content of dissolved sterols with coprostanol to cholesterin, coprostanol to cholesterin are below 0.2 respectively, indicating the water quality of underground river is not contaminated by domestic sewage, but with the passage of time water quality tends to deterioration.
Keywords:carbon sequestration  dissolved organic matter  biomarker  sterol  Qingmuguan underground river
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