Advanced Search
  • Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 32 Issue 2
Jun.  2013
Turn off MathJax
Article Contents
Article Navigation >  CARSOLOGICA SINICA  > 2013  >  32(2): 148-152
CHEN Xue bin, ZHOU Jun, LAN Jia cheng, XIAO Jing ge, YANG Ping heng. Flow field inversion of karst underground river and estimation of hydrogeological parameters based on online tracer technique[J]. CARSOLOGICA SINICA, 2013, 32(2): 148-152. doi: 10.3969/j.issn.1001-4810.2013.02.004
Citation: CHEN Xue bin, ZHOU Jun, LAN Jia cheng, XIAO Jing ge, YANG Ping heng. Flow field inversion of karst underground river and estimation of hydrogeological parameters based on online tracer technique[J]. CARSOLOGICA SINICA, 2013, 32(2): 148-152. doi: 10.3969/j.issn.1001-4810.2013.02.004
shu

Flow field inversion of karst underground river and estimation of hydrogeological parameters based on online tracer technique

doi: 10.3969/j.issn.1001-4810.2013.02.004
  • 1.

    Key Laboratory of Eco-environments in Three Gorges Reservoir Region , Ministry of Education, School of Geographical Sciences, Southwest University

  • 2.

    208 Hydrogeological Party, Bureau of Geology and Minerals Exploration of Chongqing

  • Received Date: 2012-12-19
  • Publish Date: 2013-06-25
    Abstract
  • A high-resolution online tracer test is performed in the Qingmuguan karst underground river system to get essential data for researching the morphologic features of karst underground river and estimate hydrogeological parameters. The recovery rate of the tracer is 99 %. The break-through curve of the tracer has two peaks. The first and the second peak value is respectively 37.63 and 1.21. The skewness and kurtosis of the two peaks are both greater than 0. The results of test confirmed that there is no pond developed in the Qinmuguan karst underground river. And the groundwater flow is turbulent. The paper presents empirical formulas and the formulas with practical physical meaning according to the test data and geospatial information of the underground river. The mean velocity of groundwater,friction factor, Reynolds number, Sherwood number and Schmidt number were estimated by these formulas, and the value is respectively 204 m/d, 0.26, 127 980, 4 165,1 140. These parameters show that the structure is complex in the pipeline of the Qingmuguan underground river and the environment of groundwater is vulnerable. In addition, the flow state that is represented by the estimated Reynolds number is consistent with the result that comes from concentration curve of the tracer.

     

    • FullText(HTML)
  • loading
    • References(15)
  • [1]
    杨平恒.重庆青木关地下河系统的水文地球化学特征及悬浮颗粒物运移规律［D］.重庆:西南大学，2010.
    [2]
    李敬兰，李益民.广西龙布排泥库地下水多元示踪试验研究［J］.安全与环境工程, 2004,11(1):59-62.
    [3]
    Pronk M,Goldscheider N,Zopfi J.Dynamics and interaction of organic carbon,turbidity and bacteria in a karst aquifer system ［J］.Hydrogeol Journal,2006,14(4):473-484.
    [4]
    Andreo B,Goldscheider N,Vadillo I,et al.Karst groundwater protection：First application of a Pan-European Approach to vulnerability，hazard and risk mapping in the Sierra de Libar (Southern Spain) ［J］.Sci. Total Environ., 2006, 357(1-3): 54-73.
    [5]
    Nguyet V T M, Goldscheider N.Tracer tests,hydrochemical and microbiological investigations as a basis for groundwater protection in a remote tropical mountainous karst area,Vietnam［J］.Hydrogeol Journal,2006,14(7):1147-1159.
    [6]
    Goldscheider N,Meiman J,Pronk M,et al.Tracer tests in karst hydrogeology and speleology［J］.International Journal of Speleology,2008,37(1):27-40.
    [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]
    何师意，Michele L，章程，等.高精度地下水失踪技术及其应用——以毛村地下河流域为例［J］.地球学报，2009,30(5):673-678.
    [9]
    Smart C. Artificial tracer techniques for the determination of the structure of conduit aquifers ［J］. Ground Water, 1988, 26(4): 445-453.
    [10]
    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.
    [11]
    扈志勇，杨平恒，杨梅，等. 川东槽谷区岩溶泉水物理化学变化动态特征及其环境效应研究——以重庆青木关岩溶槽谷姜家泉为例［J］.现代地质，2009,23(6):1167-1173.
    [12]
    张祯武.岩溶地下水管流场类型与示踪曲线对应关系的研究［J］.工程勘察，1991,(1):32-37.
    [13]
    杨平恒，罗鉴银，彭稳，等.在线技术在岩溶地下水示踪试验中的应用——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.
    [14]
    White W B. Geomorphology and Hydrology of Karst Terrains［M］.New York: Oxford University Press,1988:464.
    [15]
    Dreybrodt. Processes in Karst Systems［M］. New York: Springer-Verlag, 1988: 288.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 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
    Get Citation
    PDF(1640.0KB)
    XML

    Article Metrics

    Article views (2717) PDF downloads(2758) Cited by()
    Proportional views
    Related

    Website Copyright © CARSOLOGICA SINICA 桂ICP备05009877号-1

    Sponsor: Chinese Academy of Geological Sciences Sponsored by: Institute of Karst Geology, Chinese Academy of Geological Sciences Address: No.50, Qixing Road, Guilin, Guangxi

    Post Code: 541004 Tel: 0773-5812949 7796657 Email: zgyr@mail.cgs.gov.cn; zgyrbjb@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd.    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return