地震地质 ›› 2010, Vol. 32 ›› Issue (3): 473-481.DOI: 10.3969/j.issn.0253-4967.2010.03.014

• 声频大地电磁法研究与应用 • 上一篇    下一篇

线源时间域电测深全期全区视电阻率求解

赵福元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:2010-07-13 出版日期:2010-09-30 发布日期:2011-01-14
  • 通讯作者: 陈小斌,中国地震局地质研究所副研究员,联系电话:13520831459,E-mail:cxb@pku.edu.cn。
  • 作者简介:赵福元,男,1986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:13997554215,E-mail:zhao_fuyuan@163.com.
  • 基金资助:
    国家自然科学基金(40774073,40774074)资助

THE SOLUTION FOR THE ALL-TIME APPARENT RESISTIVITY IN TIME DOMAIN WITH LONG GROUND WIRE

ZHAO Fu-yuan1,2, 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:2010-07-13 Online:2010-09-30 Published:2011-01-14

摘要: 由于线源一维的正演国内外研究尚少,文中主要利用水平电场分量求取全区视电阻率。通过计算发现水平电场与电阻率之间是一一对应的关系,这使得定义全区视电阻率具有惟一性和可靠性。文中以水平电场定义视电阻率,然后利用二分搜索算法进行全区视电阻率求解。模型计算表明,该方法定义的全区视电阻率能较准确地反映地下电阻率信息。进一步研究发现:对时间域线源而言,在近区算不好晚期的数据,因为电磁波的传播、衰减很快,同样在极远区算不好早期的数据,而且探测深度是随收发距的增加而增大。最后,加入5%的随机噪声后与理论结果进行对比,得到了收发距与最大探测深度的关系。

关键词: 时间域, 全区视电阻率, 水平电场, 两分法, 随机噪声

Abstract: Because the study in line source 1-D forward is few until now,in this paper,all-time apparent resistivity is attained by horizontal component in electrical field.Theoretical calculations indicate that the horizontal electrical field component is one-to-one correspondence with resistivity,which made the definition of all-time apparent resistivity unique and reliable.The paper uses horizontal electrical field component to define the apparent resistivity and calculate with dichotomy.The calculation example shows that the apparent resistivity defined by this method can accurately reflect the information of the model.In the following research,for time domain with line source we found that at near area there are bad results from later period data.Because of the quick electromagnetic wave spread and decay,we have bad results from early stage data in far area also,and the detection depth increases with the transmitter-receiver distance.Finally,we obtain the relationship between maximum detection depth and transmitter-receiver distance by adding 5% random noise and comparing with the theoretical results.

Key words: time domain, all-time apparent resistivity, horizontal electrical field, dichotomy, random noise

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