Shadow effect and source overprint effect of short-offset transient electromagnetic method

IF 1.6 3区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Journal of Geophysics and Engineering Pub Date : 2023-03-21 DOI:10.1093/jge/gxad020
Kangxin Lei, Jinjing Shi, Weiying Chen, Wanting Song
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Abstract

In artificial-source electromagnetic explorations, shadow effect and source overprint effect are one of the key factors to affect the detection reliability. Compared with the frequency-domain electromagnetic methods, transient electromagnetic (TEM) shadow effect and source overprint effect are more complex, especially for the short-offset TEM (SOTEM) observed in the near-source region. However, there is less relevant research. Therefore, in the paper, we first realize 3D SOTEM simulations based on the vector time-domain finite element method, then further analyze the generation of SOTEM shadow effect and source overprint effect from view of the diffused electromagnetic fields, as well as their influence on ground Ex and dBz/dt responses. Results show that the attraction or repulsion of the electrical inhomogeneity would affect the diffusion speed of the electromagnetic fields, which is the essential of the two source effects. Besides, from view of the ground Ex and dBz/dt responses, the relative anomaly of SOTEM shadow effect is almost twice of those of SOTEM source overprint effect, i.e. SOTEM shadow effect is easier to be recorded, especially for the dBz/dt responses. In addition, due to the shadow effect, SOTEM may fail to identify the real target anomaly. While the influence of the source overprint effect for recognizing the target anomaly mainly occurs on all-time dBz/dt responses and early-time Ex responses (before about 10 ms), that is, observing late-time SOTEM Ex responses can effectively avoid such influence. Hence, to fully ensure avoiding the influence of the source overprint effect, we suggest adopting high-power transmission to increase the late-time signal-to-noise ratio in the field measurement.
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短偏移瞬变电磁法的阴影效应和源套印效应
在人工源电磁探测中,阴影效应和源叠加效应是影响探测可靠性的关键因素之一。与频域电磁方法相比,瞬态电磁(TEM)阴影效应和源叠加效应更为复杂,尤其是在近源区观察到的短偏移TEM。然而,相关研究较少。因此,本文首先基于矢量时域有限元方法实现了SOTEM的三维模拟,然后从散射电磁场的角度进一步分析了SOTEM阴影效应和源叠加效应的产生,以及它们对地面Ex和dBz/dt响应的影响。结果表明,电不均匀性的吸引或排斥会影响电磁场的扩散速度,这是两源效应的本质。此外,从地面Ex和dBz/dt响应来看,SOTEM阴影效应的相对异常几乎是SOTEM源叠加效应的两倍,即SOTEM阴影效果更容易被记录,尤其是对于dBz/dt的响应。此外,由于阴影效应,SOTEM可能无法识别真实的目标异常。虽然识别目标异常的源套印效应的影响主要发生在历史dBz/dt响应和早期Ex响应(大约10ms之前)上,也就是说,观察晚期SOTEM Ex响应可以有效地避免这种影响。因此,为了充分保证避免源套印效应的影响,我们建议在现场测量中采用高功率传输来提高后期信噪比。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Geophysics and Engineering
Journal of Geophysics and Engineering 工程技术-地球化学与地球物理
CiteScore
2.50
自引率
21.40%
发文量
87
审稿时长
4 months
期刊介绍: Journal of Geophysics and Engineering aims to promote research and developments in geophysics and related areas of engineering. It has a predominantly applied science and engineering focus, but solicits and accepts high-quality contributions in all earth-physics disciplines, including geodynamics, natural and controlled-source seismology, oil, gas and mineral exploration, petrophysics and reservoir geophysics. The journal covers those aspects of engineering that are closely related to geophysics, or on the targets and problems that geophysics addresses. Typically, this is engineering focused on the subsurface, particularly petroleum engineering, rock mechanics, geophysical software engineering, drilling technology, remote sensing, instrumentation and sensor design.
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