• Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 33 Issue 4
Dec.  2014
Turn off MathJax
Article Contents
YU Zheng-liang, YANG Ping-heng, GU Hai-hua, FANG Ming-yang, LI Jian-hong, CHEN Jin-long. Application of high-resolution online tracer technique in distinguishing the contaminant source of water resources in karst area: A case study of Yuquankan spring in Qianjiang county, Chongqing[J]. CARSOLOGICA SINICA, 2014, 33(4): 498-503. doi: 10.11932/karst20140415
Citation: YU Zheng-liang, YANG Ping-heng, GU Hai-hua, FANG Ming-yang, LI Jian-hong, CHEN Jin-long. Application of high-resolution online tracer technique in distinguishing the contaminant source of water resources in karst area: A case study of Yuquankan spring in Qianjiang county, Chongqing[J]. CARSOLOGICA SINICA, 2014, 33(4): 498-503. doi: 10.11932/karst20140415

Application of high-resolution online tracer technique in distinguishing the contaminant source of water resources in karst area: A case study of Yuquankan spring in Qianjiang county, Chongqing

doi: 10.11932/karst20140415
  • Publish Date: 2014-12-25
  • The high-resolution online tracer is widely employed in hydrogeology field due to its characteristics of high precision and low cost. The pollution of the Yuquankan karst spring has caused at least 3 000 local people lack of adequate healthy drinking water. In order to find out the position of the pollution sources, the high-resolution online tracer technique was applied in the survey with fluorescein sodium and tinopal as the tracers. The results show that there is a hydraulic connection between the septic tank of a livestock breeding corporation in Chongqing and the Yuquankan karst spring. The recycle proportion of fluorescein sodium is 3.51%, 2.56% for Tinopal. The breakthrough curves of both tracers show certain differences. This phenomenon may be caused by lower solubility of fluorescein sodium compaired with Tinopal. The maximum flow velocity and mean velocity of the ground water, calculated by fluorescein sodium’s first showing time and first peak appearing time, are 27.09 m/h, 22 and 32 m/h respectively, which suggests small pores and fractures and slow percolation of pollution in the Yuquankan karst spring area. The breakthrough curves are of “multi-peak type”, so at least four groundwater channels are supposed to exist between the septic tank of the livestock breeding corporation and the Yuquankan karst spring, which reflects the uniformity of fracture development of the epikarst spring.In order to recover the quality of the Yuquankan spring water, the livestock breeding corporation must take action to prevent the leakage or be shut down as soon as possible.

     

  • loading
  • [1]
    Yuan D X. Sensitivity of karst process to environmental change along the PEPII transects [J].Quaternary International,1997,37:105-113.
    [2]
    Vesper D J, Loop C M, White W B. Contaminant transport in karst aquifers [J].Theoretical and Applied Karstology,2001,13(14):101-111.
    [3]
    袁道先,朱德浩,翁金桃,等.中国岩溶学[M].北京:地质出版社,1994:129-134.
    [4]
    徐尚全,王鹏,焦杰松,等.高精度在线示踪技术在岩溶地下水文调查中的应用[J].工程勘察,2013,(2):40-44.
    [5]
    Schnegg P A,Costa R. Artificial tracer techniques of the structure of conduit aquifers[J].Ground Water,1988,26(4):445-453.
    [6]
    米德才,张新兴.浩坤水电站水库岩溶渗漏研究[J].地球与环境,2005,33(Z1):242-246.
    [7]
    邹国富,范柱国,朱春蓉,等.云南普朗铜矿尾矿库喀斯特渗漏示踪试验研究[J].成都理工大学学报(自然科学版),2009,36(3):292-297.
    [8]
    鲁程鹏,束龙仓,苑利波,等.基于示踪试验求解岩溶含水层水文地质参数[J].吉林大学学报(地球科学版),2009,39(4):717-721.
    [9]
    何师意,Michele L,章程,等.高精度地下水示踪技术及其应用:以毛村地下河为例[J].地球学报,2009,30(5):673-678.
    [10]
    Craig E D. Introduction to theme issue on tracers in hydrogeology [J].Hydrogeology Journal, 2005,13(1):255-258.
    [11]
    Schnegg P A, Costa R. Tracer tests made easier Fluorometer[J].Bulletin’ Hydrogeology Jourral, 2002,(20):89-91.
    [12]
    杨平恒,罗鉴银,彭稳,等.在线技术在岩溶地下水示踪实验中的应用:以青木关地下河系统岩口落水洞至姜家泉段为例[J].中国岩溶,2008, 27(3):215-220.
    [13]
    Field M S. The QTRACER2 program for tracer-breakthrough curve analysis for tracer tests in karstic aquifer and other hydrologic systems[M]. National Center for Environmental Assessment-Washington Office,Office of Research and Developrnent,United States Environmental Protection Agency,2002.
    [14]
    王开然,姜光辉,郭芳,等.桂林东区峰林平原岩溶地下水示踪实验与分析[J].现代地质,2013,27(2):454-459.
    [15]
    Gold S N, Meiman J, Pronk M. el al. Tracer tests in karst hydrogeology and speleology [J].International Journal of Speleology,2008,37 (1):27-40.
    [16]
    杨立铮,刘俊业.试用示踪剂浓度时间曲线分析岩溶管道的结构特征[J].成都地质学院学报,1979,16(4): 211-219.
    [17]
    陈雪彬,周军,蓝家程,等.基于在线示踪技术的岩溶地下河流畅反演与水文地质参数估算[J].中国岩溶,2013,32(2):148-152.
    [18]
    梅正星.我国喀斯特地下水示踪概况[J]. 中国岩溶,1988,7(4):371-377.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (1888) PDF downloads(1176) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return