Study of transient electromagnetic method measurements using a superconducting quantum interference device as B sensor receiver in polarizable survey area

Author:

Du Shangyu1,Zhang Yi2,Pei Yifeng2,Jiang Kun3,Rong Liangliang2,Yin Changchun4ORCID,Ji Yanju1ORCID,Xie Xiaoming2

Affiliation:

1. Jilin University, College of Instrumentation and Electrical Engineering, Changchun, China and National Engineering Research Center of Geophysics Exploration Instruments, Changchun, China..

2. Shanghai Institute of Microsystem and Information Technology (SIMIT), Chinese Academy of Sciences (CAS), State Key Laboratory of Functional Materials for Informatics, Shanghai, China and Center for Excellence in Superconducting Electronics (CENSE), Changchun, China..

3. Formerly Shanghai Institute of Microsystem and Information Technology (SIMIT), Chinese Academy of Sciences (CAS), State Key Laboratory of Functional Materials for Informatics, Shanghai, China; presently ULANTECH Co., Ltd, Shanghai, China.

4. Jilin University, College of Geo-exploration Science and Technology, Changchun, China..

Abstract

Time-domain transient electromagnetic method (TEM) measurements sometimes exhibit a sign reversal in the secondary field during the off-time, which is usually attributed to the induced-polarization (IP) effect. In contrast with the conventional IP method, which uses a current source, TEM with an ungrounded transmitting loop operates using a pure voltage source, which is induced by the primary field switching on and off. We performed TEM measurements in a resistive survey area showing an IP effect, and we used a low-temperature superconducting quantum interference device (LT-SQUID) with sensitivity of [Formula: see text] as a magnetic field sensor. A sign reversal in all of our measurements was observed; furthermore, the negative amplitude reached [Formula: see text]. In-depth analysis with an extended version of a wire-filament circuit reveals that the large negative signal may be due to discharging of in-ground capacitance, an IP effect. The conduction response of the ground can be restored by subtracting the fitted discharging response (negative valued) from the observed data. To verify this operation, we compared TEM measurements with and without wire-loop targets, which can induce a conduction field with a known decay time constant during the off-time. The extracted conduction responses of the wire-loop targets match the expected ones well. This research reveals that the primary field switch-off must always be included when interpreting TEM data with sign reversal and an LT-SQUID may be a good alternative sensor for studying the IP effect in TEM.

Funder

Shanghai Municipal Science and Technology Research Project

Jilin Province Science and Technology Development Project

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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