CN113687421B

Seismic signal data processing method and device, electronic equipment and storage medium

Abstract

The present application discloses a data processing method, device, electronic device and readable storage medium for seismic signals. The method includes filtering the original seismic signal data by using singular spectrum analysis method to obtain initial filtering data; calculating the difference and similarity between the original seismic signal data and the initial filtering data; based on the difference, similarity, preset and A weighted matrix is calculated with a weighted strength control parameter used to predict the energy decay of unstable perturbations and a local similarity threshold used to determine the degree of signal retention. Based on the weighted matrix, the original seismic signal data is filtered again to obtain the final seismic signal processing result, thereby effectively improving the signal-to-noise ratio of the seismic signal and suppressing the seismic noise more efficiently and stably.

CN113687421B, drawing sheet 1
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Term

14.9 yearsleft in the term

Expires 23 August 2041.

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  2. Granted
  3. Today
  4. Expires

6 claims: 3 independent, 3 dependent

  1. 1
    A method for processing seismic signal data, comprising:filtering original seismic signal data using a singular spectrum analysis method to obtain initial filtered data;determining the difference between the original seismic signal data and the initial filtered data similarity and similarity;a weighted matrix is calculated based on the difference, the similarity, a preset weighted strength control parameter and a local similarity threshold;the weighted strength control parameter is used to predict the energy decay of unstable disturbances, the The local similarity threshold is used to determine the degree of signal retention;the weighting matrix is used to predict the position and energy level of unstable disturbance;the original seismic signal data is filtered again based on the weighting matrix;the determination of the original The difference and similarity between the seismic signal data and the initial filtered data include: calling the absolute deviation calculation relationship to calculate the absolute deviation between the original seismic signal data and the initial filtered data u,u= [% ,j], the absolute deviation calculation relationship is: ,=4, j is the element at the position (i, j) in the absolute deviation corresponding matrix, aj is (i, j) in the original seismic signal data corresponding matrix j) the element at the position, i is the element at the position 6, j) in the corresponding matrix of the initial filtered data;call the local similarity calculation relation to calculate the local difference between the original seismic signal data and the initial filtered data Similarity V,V= , the local similarity calculation relationship is: 1. 一种地震信号的数据处理方法,其特征在于,包括: 利用奇异谱分析方法对原始地震信号数据进行滤波,得到初始滤波数据; 确定所述原始地震信号数据和所述初始滤波数据之间的差异性和相似性; 基于所述差异性、所述相似性、预先设置的加权强度控制参数和局部相似性阈值计算 加权矩阵;所述加权强度控制参数用于预测不稳定扰动的能量衰减,所述局部相似性阈值 用于确定信号保留程度;所述加权矩阵用于预测不稳定扰动的位置和能级; 基于所述加权矩阵对所述原始地震信号数据再次进行滤波处理; 所述确定所述原始地震信号数据和所述初始滤波数据之间的差异性和相似性,包括: 调用绝对偏差计算关系式计算所述原始地震信号数据和所述初始滤波数据之间的绝 对偏差u,u= [%,j],所述绝对偏差计算关系式为:,=4,j为所述绝对偏差对应矩 阵中(i, j)位置处的元素,a j为所述原始地震信号数据对应矩阵中(i, j)位置处的元素,工 为所述初始滤波数据对应矩阵中6, j)位置处的元素; 调用局部相似性计算关系式计算所述原始地震信号数据和所述初始滤波数据之间的 局部相似性V,V= ,所述局部相似性计算关系式为: Σ Σ y. . = -j ------------------------- * Xiaogongming%...N) where, Vj j is the local similarity in the corresponding matrix (i, j) the element at the position, 3 is the local smoothing window function, t is the current position (i;j) moves T units along i is also the current position (i, j) moves K units along j, d a is the element at the position (t, k) in the corresponding matrix of the original seismic signal data is the element at the position (t, k) in the corresponding matrix of the initial filtered data;The weighted intensity control parameter and the local similarity threshold are used to calculate the weighted matrix, including: calculating the weighted matrix by invoking the weighted element calculation relationship, where the weighted element calculation relationship is: (20i / ε ) r Lt. η y. . = —j —----------------------- * 小工明%…N) 式中,Vj j为局部相似性对应矩阵中(i , j)位置处的元素,3为局部平滑窗口函数,t为 当前位置(i;j)沿i移动T个单位亦为当前位置(i,j)沿j移动K个单位,d一为原始地震信号 数据对应矩阵中(t,k)位置处的元素为初始滤波数据对应矩阵中(t,k)位置处的元素; 所述基于所述差异性、所述相似性、预先设置的加权强度控制参数和局部相似性阈值 计算加权矩阵,包括: 调用加权元素计算关系式计算所述加权矩阵,所述加权元素计算关系式为: (廿i / ε ) r Lt. η w. . = ν ’J ;w..=n 'J;[1, oth erw ise 式中,Wi, j为所述加权矩阵在位置(i, j)处的元素,见, j为用于反映所述差异性的绝对偏 差对应矩阵在位置(i,j)处的元素不为归一化的绝对偏差,Vi,j为用于反映所述相似性的局 部相似性对应矩阵在位置(i , j)处的元素h为所述局部相似性阈值,P为所述加权强度控制 参数。 [1, oth erwise where, Wi, j is the element of the weighting matrix at position (i, j), see, j is the absolute deviation corresponding to the matrix used to reflect the difference at position (i, j) ) is not the normalized absolute deviation, Vi,j is the local similarity corresponding matrix used to reflect the similarity The element h at the position (i, j) is the local similarity threshold, P Control parameters for the weighted intensity.
  2. 3
    A data processing device for seismic signals, comprising:an initial filtering module for filtering original seismic signal data using a singular spectrum analysis method to obtain initial filtering data;a parameter calculation module for determining the original seismic data The difference and similarity between the signal data and the initial filtering data;a weight calculation module for calculating a weighting matrix based on the difference, the similarity, a preset weighted strength control parameter and a local similarity threshold;The weighted intensity control parameter is used to predict the energy decay of unstable disturbances, and the local similarity threshold is used to determine the degree of signal retention;the weighted matrix is used to predict the location and energy level of unstable disturbances;the denoising module, with to filter the original seismic signal data again based on the weighting matrix;the parameter calculation module is further configured to: call an absolute deviation calculation relationship to calculate the absolute difference between the original seismic signal data and the initial filtered data Deviation u,u= , the absolute deviation calculation relationship can be expressed as: outer,=h-sink J, Ui,j is the element at the position (i,j) in the absolute deviation corresponding matrix, dij is the The element at the position (i, j) in the corresponding matrix of the original seismic signal data, 5, is (i, j) in the corresponding matrix of the initial filtered data j) Elements at the position;call the local similarity calculation formula to calculate the local similarity V,V= between the original seismic signal data and the initial filtered data, and the local similarity calculation formula is: 3 . 一种地震信号的数据处理装置,其特征在于,包括: 初始滤波模块,用于利用奇异谱分析方法对原始地震信号数据进行滤波,得到初始滤 波数据; 参数计算模块,用于确定所述原始地震信号数据和所述初始滤波数据之间的差异性和 相似性; 权重计算模块,用于基于所述差异性、所述相似性、预先设置的加权强度控制参数和局 部相似性阈值计算加权矩阵;所述加权强度控制参数用于预测不稳定扰动的能量衰减,所 述局部相似性阈值用于确定信号保留程度;所述加权矩阵用于预测不稳定扰动的位置和能 级; 去噪模块,用于基于所述加权矩阵对所述原始地震信号数据再次进行滤波处理; 所述参数计算模块进一步用于: 调用绝对偏差计算关系式计算所述原始地震信号数据和所述初始滤波数据之间的绝 对偏差u,u= ,所述绝对偏差计算关系式可表示为:外,=h-汇J,Ui,j为所述绝对偏差 对应矩阵中(i,j)位置处的元素,dij为所述原始地震信号数据对应矩阵中(i, j)位置处的元 素,五,为所述初始滤波数据对应矩阵中(i, j)位置处的元素; 调用局部相似性计算关系式计算所述原始地震信号数据和所述初始滤波数据之间的 局部相似性V,V= ,所述局部相似性计算关系式为: Σ j ;Σ — —j — - ―;In the formula, Vj,j is the element at the position (i, j) in the local similarity corresponding matrix, 3 is the local smoothing window function, and T is the current position (Lj) moving along i by T The unit is also the current position (i, j) moving K units along j, dT, K is the element at the position (t, k) in the matrix corresponding to the original seismic signal data, B is the element at the position (t, k) in the matrix corresponding to the initial filtered data;the weight calculation module is further used for: calling the weighting The element calculation relational formula calculates the weighting matrix, and the weighted element calculation relational formula is: 亚明LC M%一吃) 式中,Vj,j为局部相似性对应矩阵中(i , j)位置处的元素,3为局部平滑窗口函数,T为 当前位置(Lj)沿i移动T个单位亦为当前位置(i,j)沿j移动K个单位,dT,K为原始地震信号 数据对应矩阵中(t,k)位置处的元素,乙,为初始滤波数据对应矩阵中(t,k)位置处的元素; 所述权重计算模块进一步用于: 调用加权元素计算关系式计算所述加权矩阵,所述加权元素计算关系式为: [1, o th w In the formula, Wi, j are the elements of the weighting matrix at the position (i, j), see, j is the absolute deviation used to reflect the difference. The corresponding matrix is at position (i , j) is not the normalized absolute deviation, Vi, j is the local similarity corresponding matrix used to reflect the similarity The element h at the position (i, j) is the local similarity threshold , P is the weighted intensity control parameter. [1, o th 营尸w 式中,Wi, j为所述加权矩阵在位置(i, j)处的元素,见, j为用于反映所述差异性的绝对偏 差对应矩阵在位置(i,j)处的元素不为归一化的绝对偏差,Vi,j为用于反映所述相似性的局 部相似性对应矩阵在位置(i , j)处的元素h为所述局部相似性阈值,P为所述加权强度控制 参数。
  3. 6
    6 A readable storage medium, characterized in that, a computer program is stored on the readable storage medium, and when the computer program is executed by a processor, the data processing of the seismic signal as described in any one of claims 1 to 2 is realized steps of the method. 6 .一种可读存储介质,其特征在于,所述可读存储介质上存储有计算机程序,所述计算 机程序被处理器执行时实现如权利要求1至2任一项所述地震信号的数据处理方法的步骤。