首页 | 本学科首页   官方微博 | 高级检索  
     检索      

自然电场法勘探火山岩地区地下水的研究
引用本文:张贵宾,Maurice,Aubert,齐剑玲.自然电场法勘探火山岩地区地下水的研究[J].地球物理学报,1999,42(Z1):250-256.
作者姓名:张贵宾  Maurice  Aubert  齐剑玲
作者单位:1. 中国地质大学应用地球物理系 北京 100083; 2. 法国克莱蒙第二大学地球物理观测台 克莱蒙费朗 63038; 3. 中国地质大学计算机科学系 北京 100083
基金项目:国土资源部“百名跨世纪科技人才培养计划”项目(9610)
摘    要:多个火山岩地区找水的勘探实例表明,地表观测到的自然电位异常(简称SP)与地下非饱和区厚度相关。本文认为这种自然电位异常是由于雨水垂直向下流经非饱和区(渗流区)到达地下不透水界面引起,并提出产生自然电位异常的地下极化模型,进而根据静电场理论建立了水文地质模型与自电异常之间的理论关系。这一理论能够实现把一种波数域反演技术引进自然电位异常的反演,以便计算地下水的位置和深度。模型算例和勘探实例表明这一方法可以用于勘探火山岩地区地下水。

关 键 词:火山岩地区  自然电位异常  SPS界面  地下水  
收稿时间:1999-06-17

A STUDY OF SELF-POTENTIAL METHOD IN HYDROGEOLOGICAL EXPLORATION OF VOLCANIC AREA
ZHANG GUI-BIN MAURICE AUBERT QI JIAN-LING.A STUDY OF SELF-POTENTIAL METHOD IN HYDROGEOLOGICAL EXPLORATION OF VOLCANIC AREA[J].Chinese Journal of Geophysics,1999,42(Z1):250-256.
Authors:ZHANG GUI-BIN MAURICE AUBERT QI JIAN-LING
Institution:1. Department of Geophysics, China University of Geosciences, Beijing 100083, China; 2. Observatoire de Physique duGlobe,UniversiteBlaisePascal,ClermontFerrand63038,France; 3. Department of Computer Science, China University of Geosciences, Beijing 100083, China
Abstract:Hydrogeological exploration examples of volcanic areas showed that there is a correlation between the range of negative self-potential (SP) anomaly and the thickness of the unsaturated zone measured in borings. Based on this correlation, SP anomaly is assumed to be created in the unsaturated medium through which meteoric water moves downward. A polarized model has been used to interpret SP anomaly. A formula of SP anomaly produced by the polarized model has been derived analytically. Because of the SP formula, a inverse technique in wavenumber domain can be used for inversion of the SP anomaly so as to calculate the location of ground water and the depth to ground water. The model test and the exploration example show that this method can be used to explore ground water in volcanic area.
Keywords:Volcanicarea  Self-potentialanomaly  SPSsurface  Groundwater  
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号