ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
毛坝向斜核部岩溶水绕轴径流的同位素示踪分析
  
关键词:isotopic tracing  karst water  round-axis flow  Maoba syncline
基金项目:铁道部“渝怀线圆梁山深埋特长隧道工程地质勘测”
作者单位E-mail
高志友 成都理工大学四川成都610059 cdannie@163.com 
尹观 成都理工大学四川成都610059  
蒋良文 铁道部第二勘测设计院四川成都610031  
侯明 桂林工学院广西桂林541004  
摘要点击次数: 2873
全文下载次数: 2269
摘要:
Isotopic Tracing Analysis of Round-Axis Flow of Karst Water in Maoba Syncline
      Aiming at solving the problem of karst groundwater in Maoba syncline of Yuanliangshan Tunnel,this paper deals with the formation,supply and cycling of the water by using the tracing theory of environmental isotope and deuterium excess (d-excess) parameter of groundwater. The result shows that the deep confined karst water is supplied by the water from both the east wing and the west wing of Maoba syncline. The T_1 d aquifer is mainly affected by the vertical seeping,the P_2 w+c aquifer is affected by water from the upper strata and the west wing of the syncline,and the P_1 q + m aquifer is affected by the water from F_ 02 fault and the finite seepage along the unconformable side instead of having direct hydraulic relations with the upper strata. The direction of flowing water in the syncline is from the wings to the core. The velocity of flow is slow,and there exists no round-axis flow.
GAO Zhi-you,YIN Guan,JIANG Liang-wen,HOU Ming.2004.Isotopic Tracing Analysis of Round-Axis Flow of Karst Water in Maoba Syncline[J].Acta Geoscientica Sinica,25(2):165-169.
查看全文  查看/发表评论  下载PDF阅读器
Copyright©2008 All Rights Reserved
Sponsored by:
Address:: PostCode: Tel: E-mail: