Joint Inversion of DC and TEM Methods for Geological Imaging
In this study, we present a new methodology for 2D joint inversion, or data fusion, of DC electro-resistivity and Transient Electromagnetic methods. These geophysical techniques have traditionally been used separately, but by combining them, we aim to decrease ambiguities and increase the robustness...
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Veröffentlicht in: | Pure and applied geophysics 2024-08, Vol.181 (8), p.2541-2560 |
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creator | Bortolozo, Cassiano Antonio Campaña, Julian David Realpe Santos, Fernando Acácio Monteiro Dos De Oliveira, Gabriela Serejo Porsani, Jorge Luís Pryer, Tristan Sialounas, Georgios |
description | In this study, we present a new methodology for 2D joint inversion, or data fusion, of DC electro-resistivity and Transient Electromagnetic methods. These geophysical techniques have traditionally been used separately, but by combining them, we aim to decrease ambiguities and increase the robustness of the resulting subsurface model. The inversion process was conducted using the classical Occam method with smooth models and synthetic studies were also conducted to understand the limitations and advantages of the method. We also applied the algorithm to data obtained in groundwater exploration in Brazil, and the results showed that the 2D joint inversion is promising in increasing accuracy and reducing ambiguity in subsurface imaging. |
doi_str_mv | 10.1007/s00024-024-03529-6 |
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subjects | Algorithms Aquifers Data integration Earth and Environmental Science Earth Sciences Geology Geophysical methods Geophysics/Geodesy Groundwater Groundwater data Imaging techniques Magnetic fields Methods Permeability R&D Research & development |
title | Joint Inversion of DC and TEM Methods for Geological Imaging |
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