Abstract

Magnetotelluric (MT) method is widely used for revealing deep electrical structure. However, natural MT signals are susceptible to cultural noises. In particular, the existing data-processing methods usually fail to work when MT data are contaminated by persistent or coherent noises. To improve the quality of MT data collected with strong ambient noises, we propose a novel time-series editing method based on the improved shift-invariant sparse coding (ISISC), a data-driven machine learning algorithm. First, a redundant dictionary is learned autonomously from the raw MT data. Second, cultural noises are reconstructed using the learned dictionary and the orthogonal matching pursuit (OMP) algorithm. Finally, the de-noised MT data are obtained by subtracting the reconstructed cultural noises from the raw MT data. The synthetic data, field experimental data and measured data are tested to verify the effectiveness of the newly proposed method. The results show that our new scheme can effectively remove strong cultural noises and has better adaptability and efficiency than the predefined dictionary-based methods. The method can be used as an alternative when a remote reference station is not available.

Highlights

  • The magnetotelluric (MT) method employs natural electromagnetic fields as sources, reaching a prospecting depth of 600 km or more (Simpson and Bahr 2005; Garcia et al 2015)

  • To improve the quality of MT data, we propose a novel signal–noise separation method based on the improved shift-invariant sparse coding

  • The application of the proposed method to synthetic data and real MT data shows: 1. The new scheme proposed in this paper can improve the signal–noise ratio of MT data significantly and the MT responses obtained by our method are consistent with that from the remote reference method

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Summary

Introduction

The magnetotelluric (MT) method employs natural electromagnetic fields as sources, reaching a prospecting depth of 600 km or more (Simpson and Bahr 2005; Garcia et al 2015). It is a popular and indispensable method for deep mineral resources exploration and electrical conductivity structure probing of the Earth (Guo et al 2019). Natural MT signals are weak, non-stationary and broadband in frequency, and susceptible to cultural noises (Cai et al 2009; Neukirch and Garcia 2014). As the proportion of urbanization continues to increase, the distribution of cultural noises is becoming wider and wider, which severely limits the application of the MT method

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