• Included in CSCD
  • Chinese Core Journals
  • Included in WJCI Report
  • Included in Scopus, CA, DOAJ, EBSCO, JST
  • The Key Magazine of China Technology
Volume 30 Issue 4
Dec.  2011
Turn off MathJax
Article Contents
ZHOU Xiao-ping, SHEN Li-cheng, WANG Peng, XU Shang-quan, LIN Ming-zhu. Degasification of the outcropped epikarst water:A case study on the Baishuwan Spring in Nanchuan,Chongqing[J]. CARSOLOGICA SINICA, 2011, 30(4): 432-436. doi: 10.3969/j.issn.1001-4810.2011.04.013
Citation: ZHOU Xiao-ping, SHEN Li-cheng, WANG Peng, XU Shang-quan, LIN Ming-zhu. Degasification of the outcropped epikarst water:A case study on the Baishuwan Spring in Nanchuan,Chongqing[J]. CARSOLOGICA SINICA, 2011, 30(4): 432-436. doi: 10.3969/j.issn.1001-4810.2011.04.013

Degasification of the outcropped epikarst water:A case study on the Baishuwan Spring in Nanchuan,Chongqing

doi: 10.3969/j.issn.1001-4810.2011.04.013
  • Received Date: 2011-10-17
  • Publish Date: 2011-12-25
  • HCO3- Concentration, pH, conductivity (EC) and dissolved oxygen are monitored with certain space along the downstream of the Baishuwan Spring—the Baizhi Stream, and a preliminary study on the degasification of the karst water is conducted in the case study. The results show that (1)there is a decreasing trend in HCO3- concentration along the flow path; (2) the decreasing speed of HCO3- concentration reflects the speed of degasification and the degassing speed in different season assumes “drought period > normal period > rainy period”; (3) dilution effect of the rain water makes the decreasing trend unobvious, but after the rainfall, it starts to present a decreasing trend again; (4) degasification also causes the conductivity (EC) decline along the flow path, but pH values increase; (5) diurnal variation in dissolved oxygen (DO) along the flow path shows that the aquatic organism may have some influences on the degasification, but the influencing mechanism still needs further study.

     

  • loading
  • [1]
    Broecker W S, Takahashi T, Simpppson H J, et al. Fate of fossil fuel carbon dioxide and the global carbon budget[J]. Science,1979, 206: 409-418.
    [2]
    Schindler D W. The mysterious missing sink[J]. Nature, 1999 , 398:105-106.
    [3]
    王效科,白艳莹,欧阳志云,等.全球碳循环中的失汇及其形成原因[J].生态学报,2002,22(1):94-103.
    [4]
    袁道先.现代岩溶学和全球变化研究[J].地学前沿,1997,4:17-24.
    [5]
    徐胜友,蒋忠诚.我国岩溶作用与大气温室气体CO2源汇关系的初步估算[J].科学通报,1997,42(9):953-956.
    [6]
    Adamczyk K, Prémont-Schwarz M, Pines D E, et al. Real-time observation of carbonic acid formation in aqueous solution[J],Science, 2009,326: 1690-1694.
    [7]
    Yuan Daoxian. The carbon cycle in karst[J]. Z.Geomorph, 1997,108(Suppl): 91-102.
    [8]
    李林立.西南典型岩溶生态环境对表层岩溶水调蓄功能的影响研究[D].2009.西南大学.
    [9]
    林明珠,谢世友,衡涛.喀斯特山地不同土地利用对表层岩溶泉水化学特征的影响[J].水土保持学报.2011,25(4):212-216.
    [10]
    袁道先.碳循环与全球岩溶[J].第四纪研究,1993,1:1-6.
    [11]
    刘再华,袁道先.中国典型表层岩溶系统的地球动态特征及其环境意义[J].地质论评,2000,46(3):324-327.
    [12]
    章程,袁道先,曹建华,等.典型表层岩溶泉短时间尺度动态变化[J].地球学报,2004,25(4):467-471.
    [13]
    王海静,刘再华,曾成,等.四川黄龙沟源头黄龙泉泉水及其下游溪水的水化学变化研究[J].地球化学,2009,38(3):307-314.
    [14]
    刘再华,李强,孙海龙,等.云南白水台钙华水池中水化学日变化及其生物控制的发现[J],水文地质工程地质,2005,6:10-15.
    [15]
    刘彦,张金流,何媛媛,等.单生卵囊藻对DIC的利用及其Ca-CO3沉积影响的研究[J],地球化学,2010,39(2):191-196.
  • 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 (2028) PDF downloads(916) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return