skin depth,polarization field,neural networks ,"/> GEMTIP 模型的广义趋肤深度计算及极化参数提取

吉林大学学报(信息科学版) ›› 2023, Vol. 41 ›› Issue (2): 272-280.

• • 上一篇    下一篇

GEMTIP 模型的广义趋肤深度计算及极化参数提取

史博日, 曲润祖, 刘晏廷, 邱仕林, 嵇艳鞠   

  1. (吉林大学 仪器科学与电气工程学院, 长春 130061)
  • 收稿日期:2022-03-28 出版日期:2023-04-13 发布日期:2023-04-16
  • 作者简介:史博日(2000— ), 男, 吉林榆树人, 吉林大学硕士研究生, 主要从事地磁探测方法研究, (Tel)86-15164359252(E-mail) 1351266507@ qq. com; 嵇艳鞠(1972— ) , 女, 黑龙江同江人, 吉林大学教授, 博士生导师, 主要从事时间电磁多物理场 探测理论及技术研究, (Tel)86-431-88502063(E-mail)jiyj@ jlu. edu. cn
  • 基金资助:
    国家自然科学基金重点基金资助项目(42030104) 

Research on Calculation of Generalized Skin Depth Calculation and Polarization Parameter Extraction Method of GEMTIP Model

 SHI Bori, QU Runzu, LIU Yanting, QIU Shilin, JI Yanju   

  1. (College of Instrumentation and Electrical Engineering, Jilin University, Changchun 130061, China) 
  • Received:2022-03-28 Online:2023-04-13 Published:2023-04-16

摘要: 在电磁探测过程中, 感应场和极化场并存, 如果不考虑介质的极化效应, 成像结果存在明显误差, 为此, 基于 平 面 波 理 论 和 广 义 诱 导 极 化 有 效 介 质 理 论 GEMTIP ( Generalized Effective-Medium Theory of Induced Polarization)模型, 在频域上推导了 GEMTIP 模型的广义趋肤深度公式。 通过与经典趋肤深度的比较, 验证了 GEMTIP 模型的广义趋肤深度的准确性。 GEMTIP 模型的广义趋肤深度计算主要与电阻率及体积分数有关。 采取BP(Back Propagation)神经网络反演方法进行参数提取, 通过构建合理的数据样本集, 使训练误差达到 精度要求, 得到输入输出数据之间的映射关系。 讨论了几种典型的三层地质模型结构, 在考虑极化效应时, 验证GEMTIP 模型的广义趋肤深度公式提高了地下极化介质的识别精度。

关键词: 趋肤深度, 极化场, 神经网络

Abstract:  In the field of electromagnetic detection, skin depth is an important parameter for electromagnetic data analysis and imaging. In practice, the induced field and the polarization field coexist. If the polarization effect of the medium is not considered, there will be obvious errors in the imaging results. In order to solve the above problems, the generalized skin depth formula of the GEMTIP(Generalized Effective-Medium Theory of Induced Polarization) model in the frequency domain is deduced based on the plane wave theory and the GEMTIP model. The accuracy of the generalized skin depth of the GEMTIP model is verified by comparison with the classical skin depth. The generalized skin depth calculation of the GEMTIP model is mainly related to the resistivity and volume fraction. The BP(Back Propagation) neural network inversion method is used to extract parameters. And by constructing a reasonable data sample set, the training error can meet the accuracy requirements, and the mapping relationship between the input and output data is obtained. Several typical three-layer geological model structures are discussed. When the polarization effect is considered, the generalized skin depth formula of the GEMTIP model is verified to improve the identification accuracy of the underground polarized medium. 

Key words: skin depth')">

skin depth, polarization field, neural networks

中图分类号: 

  • TP391