Abstract

We present a new tool for modelling time-lapse magnetotelluric (MT) data, an emerging technique for monitoring changes in subsurface electrical resistivity. Time-lapse MT data have been acquired in various settings, including sites of hydraulic fracturing, dewatering and sequestration. It has been shown in other geophysical techniques that the most effective way to model time-lapse data is with simultaneous inversion, which uses information from all time-steps to produce models with higher accuracy and fewer artefacts. We introduce this method to model time-lapse 1D MT data. As with a standard MT inversion, our routine penalises spatial roughness at each time-step, however we also introduce temporal regularisation. The inversion is simple to apply, requiring only the ratio between regularisation parameters and the desired level of misfit from the user. The algorithm is tested on both synthetic data, and a case study. We find that in the synthetic example our inversion successfully retrieves the main characteristics of the test model and introduces minimal artefacts, even in the presence of significant noise. We also test the effect of changing the ratio of regularisation parameters. In the case study, we produce an easily interpretable model that compares favourably with previous inversions of the synthetic data. We conclude that time-lapse modelling of 1D MT data can be a valuable tool for imaging subsurface change.

Highlights

  • In recent years, the magnetotelluric method (MT) has been increasingly used as a cost-effective technique for subsurface resistivity monitoring

  • They showed that a simultaneous inversion of Conway et al Earth, Planets and Space (2018) 70:27 time-lapse electrical resistivity tomography (ERT) data gives a superior result compared to independent inversions, cascading inversions or differenced inversions

  • We presented a simple time-lapse inversion of 1D MT data, which we tested on synthetic data and case-study data

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Summary

Introduction

The magnetotelluric method (MT) has been increasingly used as a cost-effective technique for subsurface resistivity monitoring (see Rees et al 2016, for a general introduction). Hayley et al (2011) have compared the various techniques used for inverting electrical resistivity tomography (ERT) timelapse data They showed that a simultaneous inversion of Conway et al Earth, Planets and Space (2018) 70:27 time-lapse ERT data gives a superior result compared to independent inversions, cascading inversions or differenced inversions. Their preferred technique was a special case of the 4D algorithm of Kim et al (2009), which has successfully been applied to gravity (Karaoulis et al 2013a), induced polarisation (Karaoulis et al 2013b), and seismic tomography (Karaoulis et al 2015). For each inversion the target RMS was achieved within 5 iterations, additional smoothing iterations were run, with a total of 100 iterations for each inversion

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