arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 1306.1626physics.geo-ph
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探地雷达:模拟和反演用的点衍射体分析

Ground Penetrating Radar: Analysis of point diffractors for modeling and inversion

Albane Saintenoy, A. Tarantola

摘要:

麦克斯韦方程中出现的三个电磁性质是介电常数、电导率和磁导率。对均匀各向同性线性介质中点衍射子的研究表明,可以用积分方程来描述地球电磁特性的变化。电特性(介电常数和电导率)的小的异常响应于作为电偶极子的入射电磁场,而磁特性的小的异常响应于作为磁偶极子。这两种性质的变化都不能毫无理由地忽略。考虑到不同衍射点的辐射模式,电磁变化的诊断解释在理论上是可行的,但使用探地雷达不是一件容易的任务。然而,使用有效电磁阻抗和有效电磁速度来描述介质,小异常的辐射模式表现出完全不同的源-接收器偏移。零炮检距反射波资料反映了波阻抗变化的直观图像,而大炮检距反射波资料则包含了速度变化的信息。

英文摘要:

The three electromagnetic properties appearing in Maxwell's equations are dielectric permittivity, electrical conductivity and magnetic permeability. The study of point diffractors in a homogeneous, isotropic, linear medium suggests the use of logarithms to describe the variations of electromagnetic properties in the earth. A small anomaly in electrical properties (permittivity and conductivity) responds to an incident electromagnetic field as an electric dipole, whereas a small anomaly in the magnetic property responds as a magnetic dipole. Neither property variation can be neglected without justification. Considering radiation patterns of the different diffracting points, diagnostic interpretation of electric and magnetic variations is theoretically feasible but is not an easy task using Ground Penetrating Radar. However, using an effective electromagnetic impedance and an effective electromagnetic velocity to describe a medium, the radiation patterns of a small anomaly behave completely differently with source-receiver offset. Zero-offset reflection data give a direct image of impedance variations while large-offset reflection data contain information on velocity variations.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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