CN116755165A - Ocean wave induction magnetic interference suppression and evaluation method based on time sequence matrixing - Google Patents
Ocean wave induction magnetic interference suppression and evaluation method based on time sequence matrixing Download PDFInfo
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Abstract
Description
技术领域Technical field
本发明涉及海洋地球物理信号处理技术领域,具体涉及一种基于时间序列矩阵化的海浪感应磁干扰压制和评价方法。The invention relates to the technical field of marine geophysical signal processing, and specifically relates to a method for suppressing and evaluating wave-induced magnetic interference based on time series matrixing.
背景技术Background technique
海洋大地电磁测深法(MT)通过在海底观测天然场源产生的感应电磁场获取海底介质的电性分布,它是研究海洋地壳和上地幔电性结构以及深部地质过程的重要地球物理手段。在浅水环境中,海浪运动产生的感应电磁场干扰频率范围与MT信号的频率混叠,在时域和频域都不易将其与MT信号分离;海浪感应电磁干扰具有较强的能量,极大地降低了MT数据的信噪比,导致视电阻率和相位产生严重畸变,是浅水MT数据的主要干扰。因此,需对海浪感应电磁场进行压制以提高浅水区MT数据信噪比。Marine magnetotellurics (MT) obtains the electrical distribution of the seafloor medium by observing the induced electromagnetic field generated by natural field sources on the seafloor. It is an important geophysical method for studying the electrical structure of the oceanic crust and upper mantle as well as deep geological processes. In a shallow water environment, the frequency range of the induced electromagnetic field interference generated by the movement of waves overlaps with the frequency of the MT signal, and it is difficult to separate it from the MT signal in the time domain and frequency domain; the electromagnetic interference induced by the waves has strong energy, which greatly reduces The signal-to-noise ratio of MT data is reduced, resulting in severe distortion of apparent resistivity and phase, which is the main interference of shallow water MT data. Therefore, it is necessary to suppress the wave-induced electromagnetic field to improve the signal-to-noise ratio of MT data in shallow water areas.
传统的处理方法包括小波变换、SVD分解等,由于噪声与有效信号在时域和频率混叠,上述方法容易对有效信号造成破坏,导致去噪效果不理想。于彩霞等(2010)和张宝强(2018)分别使用EMD和小波阈值去噪方法压制MT数据中的海浪感应磁噪声,这类信号分解算法能够有效改善视电阻率曲线,但相位曲线的校正效果仍不够理想。封常青等(2022)使用K-SVD字典学习算法提取海浪感应磁噪声,视电阻率畸变的改善效果明显,但相位畸变仍需借助校正后的视电阻率进行二次校正,处理效果也有待进一步提高。在去噪效果评价方面,现有方法通常在时域计算信噪比(Signal-to-Noise Ratio,SNR)、均方根误差(Root-Mean-Square Error,RMSE)和相关系数(Correlation Coefficient,CORC)等指标来评价去噪效果(Wang et al.,2017;封常青等,2022),这类指标需通过无噪信号与去噪信号做运算得到,然而,实测资料的无噪信号未知,因此这类指标无法用于实测数据的去噪效果评价。如何评价实测数据中噪声压制方法的应用效果一直是地球物理学家讨论的热点问题。Traditional processing methods include wavelet transform, SVD decomposition, etc. Due to the aliasing of noise and effective signals in the time domain and frequency, the above methods are prone to damage the effective signals, resulting in unsatisfactory denoising effects. Yu Caixia et al. (2010) and Zhang Baoqiang (2018) respectively used EMD and wavelet threshold denoising methods to suppress wave-induced magnetic noise in MT data. This type of signal decomposition algorithm can effectively improve the apparent resistivity curve, but the correction effect of the phase curve is still Less than ideal. Feng Changqing et al. (2022) used the K-SVD dictionary learning algorithm to extract wave-induced magnetic noise. The improvement effect on the apparent resistivity distortion was obvious, but the phase distortion still needs to be corrected twice with the corrected apparent resistivity, and the processing effect also needs to be Further improve. In terms of denoising effect evaluation, existing methods usually calculate the Signal-to-Noise Ratio (SNR), Root-Mean-Square Error (RMSE), and Correlation Coefficient (Correlation Coefficient) in the time domain. CORC) and other indicators to evaluate the denoising effect (Wang et al., 2017; Feng Changqing et al., 2022). Such indicators need to be obtained by calculating the noise-free signal and the denoised signal. However, the noise-free signal of the measured data is unknown , so this type of index cannot be used to evaluate the denoising effect of measured data. How to evaluate the application effect of noise suppression methods in measured data has always been a hot issue discussed by geophysicists.
发明内容Contents of the invention
本发明的目的在于提供一种基于时间序列矩阵化的海浪感应磁干扰压制和评价方法,该方法可实现单一通道时间序列数据的矩阵化,并提高海洋大地电磁数据的信噪比,提出的基于自相关函数的噪声压制效果评价方法可用于海浪磁噪声处理方法在实测数据中的应用效果。The purpose of this invention is to provide a method for suppressing and evaluating wave-induced magnetic interference based on time series matrixing. This method can realize matrixing of single-channel time series data and improve the signal-to-noise ratio of ocean magnetotelluric data. The proposed method is based on The noise suppression effect evaluation method of autocorrelation function can be used to evaluate the application effect of wave magnetic noise processing method in measured data.
为了实现以上目的,本发明提供如下技术方案:In order to achieve the above objectives, the present invention provides the following technical solutions:
1.一种基于时间序列矩阵化的海浪感应磁干扰压制和评价方法,其特征在于,包括:1. A method for suppressing and evaluating wave-induced magnetic interference based on time series matrixing, which is characterized by including:
S1、读取评价要求和海洋大地电磁场原始时间序列x(N),N为数据的个数;S1. Read the evaluation requirements and the original time series x(N) of the ocean magnetotelluric field, where N is the number of data;
S2、采用变分模态分解与带通滤波组合的方法对时间序列x(N)进行噪声估计,得到噪声时间序列xn;S2. Use the method of combining variational mode decomposition and band-pass filtering to estimate the noise of the time series x(N), and obtain the noise time series x n ;
S3、基于相空间重构矩阵化方法,从原始时间序列x(N)中抽取样本作为一维相空间矢量,构建原始时间序列矩阵XS:S3. Based on the phase space reconstruction matrix method, samples are extracted from the original time series x(N) as one-dimensional phase space vectors to construct the original time series matrix X S :
上式中,矩阵的行数m、列数n和时间延迟τ与时间序列的总数据点数N之间满足N=(m-1)τ+n,对于时间延迟τ,其取值范围为 表示向下取整;In the above formula, the relationship between the number of rows m, the number of columns n and the time delay τ of the matrix and the total number of data points N of the time series satisfies N=(m-1)τ+n. For the time delay τ, its value range is means rounding down;
S4、对估计的噪声时间序列xn进行矩阵化,得到噪声矩阵XN;S4. Matrix the estimated noise time series x n to obtain the noise matrix X N ;
S5、基于原始时间序列矩阵XS和噪声矩阵XN进行MNF变换,得到MNF成分Z;S5. Perform MNF transformation based on the original time series matrix X S and noise matrix X N to obtain the MNF component Z;
S6、基于噪声特征选择适当高阶MNF成分重构噪声矩阵 S6. Select appropriate high-order MNF components to reconstruct the noise matrix based on noise characteristics.
S7、基于时间延迟τ对重构噪声矩阵进行逆矩阵化,获得提取的噪声时间序列;S7. Reconstruct the noise matrix based on the time delay τ pair Perform inverse matrixization to obtain the extracted noise time series;
S8、估计海浪频带,对提取的噪声时间序列进行带通滤波,提取海浪感应磁噪声,从原始时间序列中减去提取的海浪感应磁噪声;S8. Estimate the wave frequency band, perform band-pass filtering on the extracted noise time series, extract the wave-induced magnetic noise, and subtract the extracted wave-induced magnetic noise from the original time series;
S9、基于压制噪声后时间序列计算自相关函数,基于自相关函数进行海浪感应磁噪声压制效果评价,自相关函数计算方法为:S9. Calculate the autocorrelation function based on the time series after suppressing the noise, and evaluate the suppression effect of wave-induced magnetic noise based on the autocorrelation function. The calculation method of the autocorrelation function is:
上式中,yt是时间序列在时刻t的观测值,是时间序列所有观测值的平均值,k是滞后时间,其取值范围为[0,N-1],自相关函数ACF就是指由自相关系数rk构成的序列;In the above formula, y t is the observed value of the time series at time t, is the average of all observations in the time series, k is the lag time, and its value range is [0, N-1]. The autocorrelation function ACF refers to the sequence composed of autocorrelation coefficients r k ;
S10、基于自相关函数判断是否满足评价要求,若满足则转向S11,若不满足则转向S3;S10. Determine whether the evaluation requirements are met based on the autocorrelation function. If so, go to S11; if not, go to S3;
S11、输出压制噪声的大地电磁时间序列。S11. Output the noise-suppressed magnetotelluric time series.
2.如权利要求1所述的基于时间序列矩阵化的海浪感应磁干扰压制和评价方法,其特征在于,MNF成分Z的计算方法为:2. The wave-induced magnetic interference suppression and evaluation method based on time series matrixing as claimed in claim 1, characterized in that the calculation method of MNF component Z is:
Z=RTXS Z = RTXS
式中,XS为原始时间序列矩阵,RT为基于噪声矩阵XN计算的构造旋转矩阵。In the formula, X S is the original time series matrix, and R T is the structural rotation matrix calculated based on the noise matrix X N.
3.如权利要求1所述的基于时间序列矩阵化的海浪感应磁干扰压制和评价方法,其特征在于,重构信号的计算方法为:3. The wave-induced magnetic interference suppression and evaluation method based on time series matrixing as claimed in claim 1, characterized in that the reconstructed signal The calculation method is:
式中,B为对m行m列的角截断矩阵,在参与重构的MNF成分的对应行上表示为1,其余部分全为0。In the formula, B is the angular truncation matrix of m rows and m columns, which is expressed as 1 on the corresponding row of the MNF component participating in the reconstruction, and the remaining parts are all 0.
4.如权利要求1所述的基于时间序列矩阵化的海浪感应磁干扰压制和评价方法,其特征在于,对重构噪声矩阵进行逆矩阵化的计算方法为基于时间延迟τ,依次消除数据矩阵中每个样本重复的数据点,并依次拼接为单一通道的时间序列。4. The wave-induced magnetic interference suppression and evaluation method based on time series matrixing as claimed in claim 1, characterized in that the reconstructed noise matrix The calculation method for inverse matrixing is based on the time delay τ, sequentially eliminating duplicate data points for each sample in the data matrix, and sequentially splicing them into a single-channel time series.
5.如权利要求1所述的基于时间序列矩阵化的海浪感应磁干扰压制和评价方法,其特征在于,基于自相关函数的噪声压制效果评价方法可应用于评价非稳定信号中有特定频率特征信号的压制效果,且可应用于实测数据评价。5. The wave-induced magnetic interference suppression and evaluation method based on time series matrixing as claimed in claim 1, characterized in that the noise suppression effect evaluation method based on the autocorrelation function can be applied to evaluate specific frequency characteristics in unstable signals. The suppression effect of the signal can be applied to the evaluation of measured data.
较现有技术相比,本发明一些实施例中,提供的方法的有益效果在于:Compared with the prior art, the beneficial effects of the method provided in some embodiments of the present invention are:
本发明主要针对海洋大地电磁探测中由海浪运动引起对MT磁场信号的强干扰,并导致大地电磁数据信噪比低的问题,提出了一种基于时间序列矩阵化的海浪感应磁干扰压制方法,该方法为复杂浅水环境下改善海洋MT资料信噪比提供了一种有效的技术方案,能够更加有效的校正相位畸变。较于传统的大地电磁噪声压制方法,该方法基于相空间重构矩阵化方法,实现单通道时间序列的矩阵化,通过最小噪声分离方法实现信号和噪声的分离,基于噪声特征选择适当高阶MNF成分重构噪声矩阵,并通过逆矩阵化,获得提取的噪声时间序列。所提出的海浪磁干扰压制方法为压制与有效信号在时域和频域混叠的噪声提供了有效解决方案,提高了大地电磁数据信噪比。This invention mainly aims at the problem of strong interference to MT magnetic field signals caused by ocean wave motion in ocean magnetotelluric detection, which leads to low signal-to-noise ratio of magnetotelluric data. It proposes a wave-induced magnetic interference suppression method based on time series matrixing. This method provides an effective technical solution for improving the signal-to-noise ratio of marine MT data in complex shallow water environments, and can more effectively correct phase distortion. Compared with the traditional electromagnetic noise suppression method, this method is based on the phase space reconstruction matrixing method to achieve the matrixing of single-channel time series, achieves the separation of signals and noise through the minimum noise separation method, and selects appropriate high-order MNFs based on noise characteristics. The components reconstruct the noise matrix, and through inverse matrixization, the extracted noise time series is obtained. The proposed wave magnetic interference suppression method provides an effective solution for suppressing the noise that overlaps with the effective signal in the time domain and frequency domain, and improves the signal-to-noise ratio of the electromagnetic data.
针对常用指标无法用于实测数据去噪效果评价的问题,提出了一种基于自相关函数的噪声压制效果评价方法,该方法结合MT信号具有非平稳特性和海浪感应磁噪声的周期性,利用二者的周期性差异评判信噪分离效果。所提出的基于自相关函数的噪声压制效果评价方法无需已知无噪信号,通过曲线的震荡形态判别去噪效果,较于传统的评价方法,这类指标可用于实测数据的去噪效果评价,提高了评价方法的应用范围和实用性。Aiming at the problem that common indicators cannot be used to evaluate the denoising effect of measured data, a noise suppression effect evaluation method based on autocorrelation function is proposed. This method combines the non-stationary characteristics of the MT signal and the periodicity of wave-induced magnetic noise, and uses two The effect of signal-to-noise separation is judged by the periodic difference between them. The proposed noise suppression effect evaluation method based on autocorrelation function does not require a known noise-free signal, and the denoising effect is judged by the oscillation shape of the curve. Compared with the traditional evaluation method, this type of index can be used to evaluate the denoising effect of measured data. The application scope and practicality of the evaluation method are improved.
附图说明Description of the drawings
为了更清楚地说明本发明实施例中的技术方案,下面将对实施例或现有技术描述中所需要使用的附图作简单地介绍,显而易见地,下面描述中的附图仅仅是本发明的部分实施例,对于本领域普通技术人员来讲,在不付出创造性劳动性的前提下,还可以根据这些附图获得其他的附图。In order to more clearly illustrate the technical solutions in the embodiments of the present invention, the drawings needed to be used in the description of the embodiments or prior art will be briefly introduced below. Obviously, the drawings in the following description are only illustrative of the present invention. For some embodiments, those of ordinary skill in the art can obtain other drawings based on these drawings without exerting any creative effort.
图1为本发明方法的程序流程框图;Figure 1 is a program flow diagram of the method of the present invention;
图2为一维地电模型结构示意图;Figure 2 is a schematic structural diagram of the one-dimensional geoelectric model;
图3为模拟MT数据加噪前后时间序列和功率谱密度图;Figure 3 shows the time series and power spectral density diagram of simulated MT data before and after adding noise;
图4为模拟MT数据去噪前后时间序列和功率谱密度图;Figure 4 shows the time series and power spectral density diagram before and after denoising the simulated MT data;
图5为模拟MT数据去噪效果自相关函数图;Figure 5 is a diagram of the autocorrelation function of the simulated MT data denoising effect;
图6为干扰压制后视电阻率及相位曲线。Figure 6 shows the apparent resistivity and phase curves after interference suppression.
具体实施方式Detailed ways
为了使本发明所要解决的技术问题、技术方案及有益效果更加清楚明白,以下结合附图及实施例,对本发明进行进一步详细说明。应当理解,此处所描述的具体实施例仅仅用以解释本发明,并不用于限定本发明。In order to make the technical problems, technical solutions and beneficial effects to be solved by the present invention clearer, the present invention will be further described in detail below with reference to the drawings and embodiments. It should be understood that the specific embodiments described here are only used to explain the present invention and are not intended to limit the present invention.
实施例1Example 1
参见图1,一种基于时间序列矩阵化的海浪感应磁干扰压制和评价方法,包括以下步骤:Referring to Figure 1, a wave-induced magnetic interference suppression and evaluation method based on time series matrixing includes the following steps:
S1、读取海洋大地电磁场原始时间序列x(N),N为数据的个数,读取评价标准,基于自相关函数的周期性特征阈值;S1. Read the original time series x(N) of the oceanic magnetotelluric field, N is the number of data, read the evaluation criteria, and the periodic characteristic threshold based on the autocorrelation function;
S2、采用变分模态分解与带通滤波组合的方法对时间序列x(N)进行噪声估计,得到噪声时间序列xn;S2. Use the method of combining variational mode decomposition and band-pass filtering to estimate the noise of the time series x(N), and obtain the noise time series x n ;
S3、基于相空间重构矩阵化方法,从原始时间序列x(N)中抽取样本作为一维相空间矢量,构建原始时间序列矩阵XS:S3. Based on the phase space reconstruction matrix method, samples are extracted from the original time series x(N) as one-dimensional phase space vectors to construct the original time series matrix X S :
上式中,矩阵的行数m、列数n和时间延迟τ与时间序列的总数据点数N之间满足N=(m-1)τ+n,对于时间延迟τ,其取值范围为 表示向下取整;In the above formula, the relationship between the number of rows m, the number of columns n and the time delay τ of the matrix and the total number of data points N of the time series satisfies N=(m-1)τ+n. For the time delay τ, its value range is means rounding down;
S4、对估计的噪声时间序列xn进行矩阵化,得到噪声矩阵XN;S4. Matrix the estimated noise time series x n to obtain the noise matrix X N ;
S5、基于原始时间序列矩阵XS和噪声矩阵XN进行MNF变换,得到MNF成分Z;S5. Perform MNF transformation based on the original time series matrix X S and noise matrix X N to obtain the MNF component Z;
S6、基于噪声特征选择适当高阶MNF成分重构噪声矩阵 S6. Select appropriate high-order MNF components to reconstruct the noise matrix based on noise characteristics.
S7、基于时间延迟τ对重构噪声矩阵进行逆矩阵化,获得提取的噪声时间序列;S7. Reconstruct the noise matrix based on the time delay τ pair Perform inverse matrixization to obtain the extracted noise time series;
S8、估计海浪频带,对提取的噪声时间序列进行带通滤波,提取海浪感应磁噪声,从原始时间序列中减去提取的海浪感应磁噪声;S8. Estimate the wave frequency band, perform band-pass filtering on the extracted noise time series, extract the wave-induced magnetic noise, and subtract the extracted wave-induced magnetic noise from the original time series;
S9、基于压制噪声后时间序列计算自相关函数,基于自相关函数进行海浪感应磁噪声压制效果评价,自相关函数计算方法为:S9. Calculate the autocorrelation function based on the time series after suppressing the noise, and evaluate the suppression effect of wave-induced magnetic noise based on the autocorrelation function. The calculation method of the autocorrelation function is:
上式中,yt是时间序列在时刻t的观测值,是时间序列所有观测值的平均值,k是滞后时间,其取值范围为[0,N-1],自相关函数ACF就是指由自相关系数rk构成的序列;若存在海浪感应磁噪声影响,则MT时间序列的ACF曲线表现出一定的周期性波动;若海浪感应磁噪声被压制,则ACF曲线中的周期性波动消减,表现为一条较光滑的曲线。基于上述特征,ACF可用于评价实测MT数据的去噪效果;In the above formula, y t is the observed value of the time series at time t, is the average of all observations in the time series, k is the lag time, and its value range is [0, N-1]. The autocorrelation function ACF refers to the sequence composed of autocorrelation coefficients r k ; if there is wave-induced magnetic noise If affected, the ACF curve of the MT time series shows certain periodic fluctuations; if the wave-induced magnetic noise is suppressed, the periodic fluctuations in the ACF curve are reduced and appear as a smoother curve. Based on the above characteristics, ACF can be used to evaluate the denoising effect of measured MT data;
S10、基于自相关函数判断是否满足评价要求,若满足则转向S11,若不满足则转向S3;S10. Determine whether the evaluation requirements are met based on the autocorrelation function. If so, go to S11; if not, go to S3;
S11、输出压制噪声的大地电磁时间序列。S11. Output the noise-suppressed magnetotelluric time series.
实施例2Example 2
参考图2,为一维地电模型图。为验证本发明所提出压制实测海浪感应磁干扰的可行性,以图2所示一维海洋地电模型模拟的磁场作为有效磁信号,以合成海浪感应磁场作为噪声并混入有效信号中,实现在海浪感应磁干扰影响频带内有效信号和噪声混叠。利用二维随机海浪感应磁场公式模拟海浪感应磁噪声。假定海浪谱为PM谱,地磁场强度为48000nT,海水层厚度为25m,磁偏角60°,磁倾角45°,海水电阻率为0.3Ω·m,风速为13m/s,模拟得到采样率为10Hz,时长为1h的海浪感应水平磁场时间序列。将模拟海浪感应磁噪声加入的模拟海洋大地电磁分量中,得到合成MT数据。图3为加噪前后MT时间序列及功率谱密度。由图可见,加噪后MT数据的功率谱密度在0.1Hz附近出现了强能量异常凸起,该异常即为海浪感应磁噪声。图4为本发明所述方法的去噪结果。由图可见,经MNF去噪后的时间序列与无噪MT信号的拟合程度高,MNF可以在压制海浪感应磁噪声的同时较好地保护MT信号,表现出较强的信噪分离能力。Refer to Figure 2, which is a one-dimensional geoelectric model diagram. In order to verify the feasibility of suppressing the measured wave-induced magnetic interference proposed in this invention, the magnetic field simulated by the one-dimensional ocean geoelectric model shown in Figure 2 is used as the effective magnetic signal, and the synthesized wave-induced magnetic field is used as noise and mixed into the effective signal to achieve Wave-induced magnetic interference affects the aliasing of effective signals and noise in the frequency band. The two-dimensional random wave-induced magnetic field formula is used to simulate wave-induced magnetic noise. Assume that the wave spectrum is a PM spectrum, the geomagnetic field intensity is 48000nT, the seawater layer thickness is 25m, the magnetic declination angle is 60°, the magnetic inclination angle is 45°, the seawater resistivity is 0.3Ω·m, and the wind speed is 13m/s, the simulation results in a sampling rate 10Hz, 1h wave-induced horizontal magnetic field time series. The simulated wave-induced magnetic noise is added to the simulated ocean magnetotelluric component to obtain synthetic MT data. Figure 3 shows the MT time series and power spectral density before and after adding noise. It can be seen from the figure that the power spectral density of the MT data after adding noise has a strong energy anomaly bulge near 0.1Hz. This anomaly is the wave-induced magnetic noise. Figure 4 is the denoising result of the method of the present invention. It can be seen from the figure that the time series denoised by MNF has a high degree of fit with the noise-free MT signal. MNF can better protect the MT signal while suppressing the magnetic noise induced by waves, showing strong signal-to-noise separation capabilities.
图5为评价合成MT数据去噪效果的自相关函数ACF图,该图展示了去噪前后MT数据及模拟海浪感应磁噪声的ACF曲线,图中虚线指示去噪前合成MT数据ACF曲线峰值所在的滞后时间k,已知合成MT数据的采样率f=10Hz,计算得到两峰值之间的时间间隔Δt=Δk/f。由图可见,模拟海浪感应磁噪声的ACF曲线表现出明显的周期性波动特征且在小滞后时间处更明显,而无噪MT信号的ACF曲线为一条平缓下降的光滑曲线。在海浪感应磁噪声的影响下,合成MT数据的ACF曲线出现相应的周期性波动特征,且峰值出现的周期在海浪感应磁噪声的周期范围(6~16s)内。MNF处理结果的ACF曲线与无噪MT信号的ACF曲线几乎完全重合,周期性波动特征消失,说明MNF在压制海浪感应磁噪声的同时对MT信号的损伤较小。Figure 5 is an autocorrelation function ACF diagram to evaluate the denoising effect of synthetic MT data. The diagram shows the ACF curve of MT data before and after denoising and the simulated wave-induced magnetic noise. The dotted line in the diagram indicates the peak of the ACF curve of the synthetic MT data before denoising. The lag time k, the sampling rate of the synthetic MT data is known to be f = 10 Hz, and the time interval between the two peaks Δt = Δk/f is calculated. It can be seen from the figure that the ACF curve simulating the magnetic noise induced by sea waves shows obvious periodic fluctuation characteristics and is more obvious at small lag times, while the ACF curve of the noiseless MT signal is a smooth curve that decreases gently. Under the influence of wave-induced magnetic noise, the ACF curve of the synthesized MT data shows corresponding periodic fluctuation characteristics, and the period of peak occurrence is within the period range of wave-induced magnetic noise (6-16 s). The ACF curve of the MNF processing result almost completely coincides with the ACF curve of the noiseless MT signal, and the periodic fluctuation characteristics disappear, indicating that MNF suppresses the magnetic noise induced by sea waves while causing less damage to the MT signal.
对压制海浪感应磁噪声前后的合成MT数据进行Robust阻抗估计,并计算得到视电阻率曲线和相位曲线如图6所示。由图可知,对于加入海浪感应磁噪声的合成MT数据,其视电阻率和相位曲线在6-16s周期范围内出现了畸变,明显偏离了真实值。经过MNF处理得到的视电阻率曲线和相位曲线更光滑连续,在受海浪干扰影响的频带,在数值上与真实值更接近。模拟数据处理结果表明,本发明所提出算法可以有效压制磁场分量中混叠的实测海浪感应磁场,通过估算阻抗并最终得到更加可靠的视电阻率及相位曲线。由此也说明,本发明提出的算法是有效的。Robust impedance estimation was performed on the synthetic MT data before and after suppressing the wave-induced magnetic noise, and the apparent resistivity curve and phase curve were calculated as shown in Figure 6. It can be seen from the figure that for the synthetic MT data with added wave-induced magnetic noise, the apparent resistivity and phase curves are distorted in the 6-16s period range, significantly deviating from the true values. The apparent resistivity curve and phase curve obtained after MNF processing are smoother and more continuous, and in the frequency band affected by wave interference, they are numerically closer to the true value. The simulation data processing results show that the algorithm proposed in the present invention can effectively suppress the measured wave-induced magnetic field mixed in the magnetic field component, and finally obtain more reliable apparent resistivity and phase curves by estimating the impedance. This also shows that the algorithm proposed by the present invention is effective.
以上所述仅为本发明的较佳实施例而已,并不用以限制本发明,凡在本发明的精神和原则之内所作的任何修改、等同替换和改进等,均应包含在本发明的保护范围之内。The above descriptions are only preferred embodiments of the present invention and are not intended to limit the present invention. Any modifications, equivalent substitutions and improvements made within the spirit and principles of the present invention shall be included in the protection of the present invention. within the range.
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