检索表面核磁共振测量中谐波干扰多基频的高效算法

R. Ghanati, Trevor Irons, Mohammad Reza Hatami
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摘要

通过地表核磁共振测量成功恢复水文地质物理参数取决于信号的质量,而在城市地区,基频不同的多个噪声源产生的谐波会显著降低信号的质量。谐波基频的准确估计是基于谐波噪声消除方法的主要步骤。现有的基于一维和二维模型的方法涉及一个计算昂贵的过程,为处理大型地表核磁共振数据集设置了限制。此外,经典的 Nyman、Gaiser 和 Saucier 估计(NGSE)算法尽管执行速度很快,但在事先不知道真实基频与其标称值之间频率偏移的预期值时,可能无法准确恢复谐波成分。由于缺乏相关知识,很难准确估计谐波的最大次数,从而导致基频恢复不准确。为了克服这些局限性,我们提出了一种基于高效最大谐波数搜索方法的增强版 NGSE 方法,用于处理受电力线谐波干扰的单频和多频表面 NMR 信号。我们在嵌入模拟电力线谐波信号的合成数据集、真实电磁噪声记录以及真实表面核磁共振数据集上验证了算法的效率。我们的数值实验证实,与基于模型的方法相比,根据信号是否具有单频、双频或三频内容,所提出的算法可以同时检索多个基频,在总体计算时间上显著加快 4 到 87 倍。
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An Efficient Algorithm to Retrieve Multiple Fundamental Frequencies of Harmonic Interference in Surface-NMR Measurements
The successful recovery of hydrogeophysical parameters through surface-NMR measurements depends on the quality of the signal, which can be significantly degraded by harmonics from multiple noise sources with different fundamental frequencies in urban areas. Accurate estimation of the fundamental frequencies of harmonics is the main step in harmonic noise cancellation-based methods. The existing 1D and 2D model-based approaches involve a computationally expensive process that sets limits for processing of large surface-NMR data sets. In addition, the classical Nyman, Gaiser, and Saucier estimation (NGSE) algorithm, despite its fast implementation, may not accurately recover harmonic components when there is no prior knowledge of the expected value of the frequency offset between the true fundamental frequencies and their nominal values. This lack of knowledge can make it difficult to accurately estimate the maximum number of harmonics and, consequently, result in an incorrect recovery of the fundamental frequency. To surmount these limitations, we propose an enhanced version of the NGSE approach based on an efficient maximum number of harmonics search approach to process surface-NMR signals corrupted by powerline harmonics with both single and multiple frequency content. We verify the efficiency of our algorithm on a synthetic dataset embedded in simulated powerline harmonic signals, and real electromagnetic noise recordings, as well as a real surface-NMR data set. Our numerical experiments confirm that the proposed algorithm can retrieve the multiple fundamental frequencies simultaneously with a significant speedup ranging from 4 to 87 times, depending on whether the signal has single, dual, or triple frequency content, in the overall computation time compared to the model-based methods.
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