吉林大学学报(地球科学版) ›› 2022, Vol. 52 ›› Issue (3): 754-765.doi: 10.13278/j.cnki.jjuese.20210242

• 第十五届中国国际地球电磁学术研讨会专栏 • 上一篇    下一篇

起伏地形条件下长偏移距瞬变电磁三维正演

王新宇1, 2, 严良俊1, 2, 毛玉蓉1, 2, 黄鑫1, 2, 谢兴兵1, 2, 周磊1, 2   

  1. 1.油气资源与勘探技术教育部重点实验室(长江大学),武汉430100

    2.非常规油气省部共建协同创新中心,武汉430100

    1.  Key Laboratory of Exploration Technologies for Oil and Gas Resources (Yangtze University), Ministry of Education, Wuhan 430100, China

    2. Cooperative Innovation Center of Unconventional Oil and Gas, Wuhan 430100, China

  • 出版日期:2022-05-26 发布日期:2024-01-03
  • 基金资助:

    国家自然科学基金项目(42030805,41774082);湖北省教育厅科学技术研究计划青年人才项目(Q20201311)

Three-Dimensional Forward Modeling of Long-Offset Transient Electromagnetic Method over Topography

Wang Xinyu1, 2, Yan Liangjun1, 2, Mao Yurong1, 2, Huang Xin1, 2, Xie Xingbing1, 2, Zhou Lei1, 2   

  1. 1.  Key Laboratory of Exploration Technologies for Oil and Gas Resources (Yangtze University), Ministry of Education, Wuhan 430100, China

    2. Cooperative Innovation Center of Unconventional Oil and Gas, Wuhan 430100, China

  • Online:2022-05-26 Published:2024-01-03
  • Supported by:
    Supported by the National Natural Science Foundation of China (42030805, 41774082) and the Science and Technology Research Program of Hubei Provincial Department of Education (Q20201311)

摘要: 地球物理勘探区的地形往往是起伏复杂的,传统长偏移距瞬变电磁法(long-offset transient electromagnetic method, LOTEM)三维正演模拟一般不考虑地形的影响,而地形因素会严重影响LOTEM数据的合理解释。因此,本文开展起伏地形条件下非结构矢量有限元LOTEM三维正演模拟。首先,应用三维建模软件Blender准确建立复杂地电模型,采用非结构四面体网格精细刻画起伏地形。其次,基于偶极子离散的长导线源近似技术,将长导线源离散为若干段等效电偶极子,并引入二阶后退欧拉格式完成时间离散。进而实现LOTEM快速、高精度三维正演。在保证计算精度的前提下,模拟了起伏地形条件下复杂地质模型的瞬变电磁场响应。模拟结果表明,由于地形的影响,LOTEM电磁场响应“畸变”严重,会削弱甚至完全“埋没”地下异常体的瞬变电磁场响应,严重影响地下目标体的有效探测。

关键词: 长偏移距瞬变电磁法, 起伏地形, 非结构矢量有限元, Blender, 二阶后退欧拉格式, 三维正演

Abstract:

The topography of geophysical exploration areas is often undulating and complex, and the traditional long-offset transient electromagnetic method (LOTEM) 3D forward modeling generally does not consider the influence of topography. However, the topographic factors seriously affect the reasonable interpretation of LOTEM data. The 3D forward modeling of LOTEM under real topography by the unstructured edge finite element method is developed in this study. Firstly, the 3D modeling software Blender is used to accurately build a complex geoelectric model, and the unstructured tetrahedral mesh is used to finely describe the real topography. Secondly, the dipole discrete field source processing technique is used to separate the long conductor source into several electric dipoles, and the second-order backward-Euler scheme is used to complete the time discretization. In this way, fast and high precision 3D forward modeling of LOTEM can be realized. The transient electromagnetic field response characteristics of the complex geological model under real topography conditions are simulated on the premise of guaranteed computational accuracy. The results demonstrate that due to the influence of topography, the LOTEM electromagnetic field response is severely “distorted”, which can weaken or even completely “cover up” the transient electromagnetic field response of underground targets, and it seriously affects the effective detection of underground targets.

Key words: long-offset transient electromagnetic method, topography, unstructured edge finite element method, Blender, second-order backward-Euler scheme, 3D forward modeling

中图分类号: 

  • P631
[1] 齐彦福, 李貅, 孙乃泉, 戚志鹏, 周建美, 张明晶, 邢涛. 电性源短偏移距瞬变电磁地形影响特征分析[J]. 吉林大学学报(地球科学版), 2022, 52(1): 247-.
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[3] 赵广茂,李桐林,王大勇,李建平. 基于二次场二维起伏地形MT有限元数值模拟[J]. J4, 2008, 38(6): 1055-1059.
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