J4 ›› 2009, Vol. 39 ›› Issue (4): 717-721.

• 地质工程与环境工程 • 上一篇    下一篇

基于示踪试验求解岩溶含水层水文地质参数

鲁程鹏1|束龙仓1|苑利波2,张蓉蓉1|黄币娟1|王彬彬1   

  1. 1.河海大学 水文水资源与水利工程科学国家重点实验室|南京 210098;2.辽宁工程勘察院,辽宁 锦州 121001
  • 收稿日期:2008-10-24 出版日期:2009-07-26 发布日期:2009-07-26
  • 通讯作者: 束龙仓(1964-),男,安徽无为人,教授,博士生导师,主要从事地下水系统模拟及控制、地下水与地表水相互作用研究 E-mail:lcshu@hhu.edu.cn
  • 作者简介:鲁程鹏(1984-)|男|安徽肥东人|博士研究生|主要从 事多重介质水流运动规律研究、水文不确定性研究|E-mail:thebest@hhu.edu.cn
  • 基金资助:

    国家“973”计划项目(2006CB403200);高等学校学科创新引智计划项目(B08048);教育部长江学者和创新团队发展计划(IRT0717)

Determination of Hydrogeologic Parameters of Karst Aquifer Based on Tracer Test

LU Cheng-peng1,SHU Long-cang1,YUAN Li-bo2|ZHANG Rong-rong1,HUANG Bi-juan1,WANG Bin-bin1   

  1. 1.State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China;2.Liaoning Institute of Engineering Exploration|Jinzou, Liaoning 121001|China
  • Received:2008-10-24 Online:2009-07-26 Published:2009-07-26

摘要:

示踪试验作为重要的水文地质试验,长久以来以探明地下水的水力联系、测定地下水流速为主要目标。针对岩溶地区地下水流速较快的特点,提出了一套基于对流稀释作用的数学模型,利用电导率与溶质浓度的正相关关系,可方便准确地计算示踪试验投源井的天然径流量和地下水中示踪剂的背景浓度。根据后寨地下河流域陈旗典型试验区的计算成果,投源井的天然径流量为0.241 4 m3/min,辅以必要的水文地质调查,即可估算地下水流速以及含水层的渗透系数。

关键词: 示踪试验, 天然径流量, 对流稀释, 水文地质参数

Abstract:

Tracer test as an important hydrogeology test, are widely used to explore the hydraulic connectivity underground, measure the groundwater flow velocity. According to the fast flow in karst aquifer, a mathematic model based on the dilution function of convection is proposed. By means of this model and the linear relationship between electricity conductivity and solution concentration, the authors can easily and accurately calculate the groundwater runoff of source well and the tracer concentration in the original groundwater. In this case study, the runoff of source well which in Chenqi of Houzhai underground river basin is 0.241 2 m3/min. Furthermore, supplemented with necessary hydrogeology investigation, the groundwater flow velocity and aquifer conductivity can be estimated.

Key words: tracer test, groundwater runoff, convection dilution, hydrogeological parameters

中图分类号: 

  • P641.134
[1] 束龙仓, 许杨, 吴佩鹏. 基于MODFLOW参数不确定性的地下水水流数值模拟方法[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1803-1809.
[2] 赵良杰, 夏日元, 易连兴, 杨杨, 王喆, 卢海平. 基于流量衰减曲线的岩溶含水层水文地质参数推求方法[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1817-1821.
[3] 卞建民, 姜振蛟, 张丽姝. 含水层中弥散系数的尺度效应[J]. J4, 2012, 42(4): 1159-1165.
[4] 曹剑峰,沈媛媛,平建华,杜全友,刘梅侠. 地下水化学动力学法在大庆前进水源地求参中的应用[J]. J4, 2006, 36(01): 96-0102.
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