地震地质 ›› 2010, Vol. 32 ›› Issue (3): 465-472.DOI: 10.3969/j.issn.0253-4967.2010.03.013

• 声频大地电磁法研究与应用 • 上一篇    下一篇

频率域线源近区(过渡区)测深理论初步研究

周磊1,2, 严良俊1, 何展翔2, 陈小斌3   

  1. 1. 长江大学, 油气资源与勘探技术教育部重点实验室, 湖北荆州, 434023;
    2. 东方地球物理公司综合物化探研究生工作站, 涿州, 072751;
    3. 中国地震局地质研究所, 北京, 100029
  • 收稿日期:2010-03-04 修回日期:2010-07-10 出版日期:2010-09-30 发布日期:2011-01-14
  • 通讯作者: 陈小斌,副研究员,电话:13520831459,E-mail:cxb@pku.edu.cn。
  • 作者简介:周磊,男,1985年生,长江大学地球探测与信息技术专业在读硕士研究生,主要研究方向为电法勘探及数值模拟,电话:13986721795,E-mail:zhoulei-85-7-8@163.com.
  • 基金资助:
    国家自然科学基金(40774073,40774074)资助

A PRIMARY STUDY ON THE FREQUENCY DOMAIN SOUNDING METHOD IN NEAR FIELD WITH LONG GROUNDED WIRE

ZHOU Lei1,2, YAN Liang-jun1, HE Zhan-xiang2, CHEN Xiao-bin3   

  1. 1. Yangtze University, Key Laboratory of Exploration Technologies for Oil and Gas Resources, Jingzhou 434023, Hubei, China;
    2. Graduate Student Studio, Department of Integrative Geophysical and Geochemical Exploration, BGP, Zhuozhou 072751, China;
    3. Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • Received:2010-03-04 Revised:2010-07-10 Online:2010-09-30 Published:2011-01-14

摘要: 对频率域无限长线源近区(过渡区)测深的理论基础进行了探索性研究。通过计算均匀半空间、层状介质等多个模型的线源响应,进而定义并计算全区视电阻率。结果发现,利用水平电场、垂直磁场分别计算的全区视电阻率均能较好地反映地下电性结构的变化。把水平磁场与水平电场联合通过二分搜索算法计算的全区视电阻率也能较好地反映地下电性结构的变化。在近区通过单分量定义的全区视电阻率与一维MT曲线吻合得很好,因此可以用成熟的MT反演技术来进行线源近区电磁资料的反演,从而把有源的问题转化到无源的问题。这初步表明频率域线源近区(过渡区)测深是可行的,但还有一些问题需要解决。

关键词: 线源, 近区(过渡区), 全区视电阻率, 层状介质

Abstract: The preliminary research result of electromagnetic prospecting of the near field(transition region) of long grounded wire in frequency domain is presented in this paper.And the full-region apparent resistivity is defined and calculated from some modeling results including the response of half space and the response of stratified space.From the results,we get the conclusion that the full-region apparent resistivity in the above situation defined from horizontal electric field and vertical magnetic field can yield a good outcome of underground electric structure.The full-region apparent resistivity calculated by using dichotomy after joining horizontal magnetic field and horizontal electrical field together can also reflect the change of electric structure underground.The full-region apparent resistivity defined by using a single component in the near field matches well with the single dimensional MT curve,therefore,mature MT inversion technology can be used to do the inversion of the near field,thus transforming the function with source to non-source types.It is available to prospect in the near field(transition region) with long grounded wire,even there are still some pending problems.

Key words: line source, near field(transition region), full-region apparent resistivity, stratified media

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