Sensitivity analysis of inverted model parameters from transient electromagnetic measurements affected by induced polarization effects

灵敏度(控制系统) 瞬态(计算机编程) 极化(电化学) 激发极化 瞬态分析 机械 声学 物理 瞬态响应 电子工程 工程类 计算机科学 电气工程 化学 操作系统 物理化学 电阻率和电导率 量子力学
作者
Lukas Aigner,Dieter Werthmüller,Adrián Flores Orozco
出处
期刊:Journal of Applied Geophysics [Elsevier BV]
卷期号:223: 105334-105334 被引量:6
标识
DOI:10.1016/j.jappgeo.2024.105334
摘要

<p>We investigate the application of the distance-based global sensitivity analysis (DGSA) to evaluate the sensitivity of electrical model parameters obtained from transient electromagnetic (TEM) data including induced polarization (IP) effects. We propose novel open-source forward modeling and inversion routines for single-loop TEM data including IP effects with the maximum phase angle model to model the frequency dependence of the complex resistivity. In a first step, we evaluate the accuracy of our forward modeling and inversion routines using numerical studies, where the actual variations of layer thicknesses and resistivities, as well as the frequency dependence of the complex resistivity is known. In a second step, we extend our investigation to field data and apply our approach to three distinct case studies in layered media: 1) a confined aquifer corresponding to conductive non-polarizable media, 2) a graphite deposit corresponding to highly conductive and polarizable anomalies in a resistive host rock and 3) an ice glacier corresponding to highly resistive polarizable media. Our DGSA results reveal that standard depth of investigation (DOI) approaches may overestimate the true sensitivity of the model obtained from the inversion. TEM data collected in conductive layered media without IP effects show reduced sensitivity above the predicted DOI. The case studies in polarizable media demonstrate that the maximum phase angle is more influential on the TEM model response than the relaxation time and dispersion coefficient. Our DGSA results for polarizable media reveal that TEM field data collected at the graphite deposit and at the ice glacier are sensitive to the geometry of the polarizable layer.</p>
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