基于高斯过程回归的瞬变电磁信号去噪方法

A Gaussian process regression-based denoising method for transient electromagnetic signals

  • 摘要:
    目的 瞬变电磁法是当前探测煤田地下水的主要地球物理方法,探测结果直接影响煤矿防治水工作的开展。针对数据采集过程难以避开输电线路等电磁干扰源,瞬变信号容易混入电磁噪声,而主要的小波变换、经验模态分解去噪技术尚需进一步改进的客观现状,提出一种基于高斯过程回归的瞬变电磁信号去噪新方法。
    方法 对含噪信号进行时间补偿,使信号幅值处于基本相当的幅度;采用径向基函数核对时间补偿后的信号进行非参数回归拟合,捕捉信号非线性趋势并分离噪声;恢复时间补偿得到去噪结果。
    结果 (1)对分别添加正弦噪声、三角波噪声、均匀噪声和高斯噪声4种单类型噪声的瞬变电磁理论信号进行去噪后,信噪比提升24.61 dB~36.03 dB,平均相对误差降低5.93%~9.06%;(2)对分别添加2种混合噪声的瞬变电磁信号去噪后,信噪比分别提升28.05 dB、26.92 dB,平均相对误差分别降低5.22%、8.35%;(3)现场实验数据去噪结果相比含噪信号的信噪比提升18.76 dB,平均相对误差降低175.92%,实验点感应曲线中噪声的振荡影响被大幅消除,实验线反演电阻率断面恢复了地层的纵向地电结构和横向连续性,与无噪实验结果基本一致,相对小波变换结果有明显提升。
    结论 基于高斯过程回归的去噪算法对含有理论噪声或现场实验噪声的瞬变电磁信号,均取得了较为明显的去噪效果,可改进其协方差函数以进一步提高去噪效果,并在生产工作中应用。研究成果为瞬变电磁信号去噪提供了新手段并具有实用价值。

     

    Abstract:
    Objective The transient electromagnetic (TEM) method serves as a primary geophysical technique for groundwater detection in coalfields at present, with the detection results directly influencing the implementation of water hazard prevention and control in coal mines. Since it is difficult to avoid electromagnetic interference sources such as power lines during data acquisition, TEM signals are prone to be contaminated by electromagnetic noise. Given that primary denoising techniques such as wavelet transform and empirical mode decomposition (EMD) are yet to be further improved, this study developed a novel Gaussian process regression (GPR)-based denoising method for TEM signals.
    Methods First, time alignment was applied to the noisy TEM signals to ensure roughly equivalent signal magnitudes. Next, non-parametric regression-based fitting was performed for the aligned TEM signals using the radial basis function (RBF), aiming to capture the non-linear trend of the signals and separate noise. Finally, temporal alignment was reversed to obtain the final denoising results.
    Results For theoretical TEM signals contaminated by four types of individual noise (e.g., sinusoidal, triangular wave, uniform, and Gaussian noise), the proposed method increased their signal-to-noise ratios (SNRs) by 24.61 dB‒36.03 dB and decreased their mean relative errors (MREs) by 5.93%‒9.06%. For TEM signals contaminated by two types of mixed noise, the proposed method increased their SNRs by 28.05 dB and 26.92 dB and decreased their MREs by 5.22% and 8.35%. For field experimental data from a coalfield, the new method increased their SNR by 18.76 dB and decreased their MRE by 175.92%. The oscillatory effects of noise in the induction curves of the survey points were significantly eliminated. Furthermore, the inverted resistivity sections of the survey line exhibited restored longitudinal geoelectric structures and lateral continuity of the strata. The experimental results were roughly consistent with those of noise-free TEM signals. Compared to the wavelet transform, the proposed method exhibited a significant improvement in the denoising results.
    Conclusions The GPR-based denoising algorithm yields significant denoising results for TEM signals contaminated by theoretical or field experimental noise. For practical applications, its denoising effect can be further improved by improving its covariance function. The results of this study provide a novel, practical solution for the TEM signal denoising.

     

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