以多道面波分析技术(MASW)为代表的主动源面波方法已经在地表勘探领域获得越来越多的应用.准确的面波相速度频散成像是利用主动源面波法进行近地表横波速度反演的必要条件.本文提出了一种新的主动源面波频散成像方法—CCPS(Cross-Correl...以多道面波分析技术(MASW)为代表的主动源面波方法已经在地表勘探领域获得越来越多的应用.准确的面波相速度频散成像是利用主动源面波法进行近地表横波速度反演的必要条件.本文提出了一种新的主动源面波频散成像方法—CCPS(Cross-Correlation and Phase-Shifting)法.首先,将单炮面波记录由时空域变换到频率空间域并消去振幅谱的影响,得到归一化频谱.然后,依次将每道信号与整个记录进行互相关的同时进行相速度扫描叠加.最后经过一次求和过程即得到最终的频散图像.通过理论数据、实际工程地震面波资料和石油勘探面波资料比较了普通相移法和CCPS法的频散成像效果.研究表明:新方法相对于普通相移法而言,明显提高了频散图像的质量,相速度聚焦性能和背景噪声压制能力有显著改善.展开更多
准确的相速度频散图像是主动源面波勘探方法反演近地表横波速度的基础。提出了一种基于频率-速度域多重信号分类(multiple signal classification in frequency-velocity domain)的面波高分辨率频散成像方法(简称fv-MUSIC方法)。该方法...准确的相速度频散图像是主动源面波勘探方法反演近地表横波速度的基础。提出了一种基于频率-速度域多重信号分类(multiple signal classification in frequency-velocity domain)的面波高分辨率频散成像方法(简称fv-MUSIC方法)。该方法首先将传统的频率-波数域波束形成器改造成频率-速度域形式,然后引入多重信号分类算法将空间谱相关矩阵分解为信号子空间和噪声子空间两个部分,最后利用噪声子空间部分生成最终的面波频散图像。理论数据和实际数据应用结果表明,该方法能产生较高精度的相速度图像,并且使用方便,计算效率高,尤其当接收排列较短时,该方法依然能保持较高的相速度分辨率,有利于提高主动源面波方法的横向速度分辨能力。展开更多
Polarity reversals may occur to transmitted P waves if the incidence angle is greater than the critical incidence angle. We analyze the characteristics of reflection and transmission coefficients under the condition o...Polarity reversals may occur to transmitted P waves if the incidence angle is greater than the critical incidence angle. We analyze the characteristics of reflection and transmission coefficients under the condition of wide incidence angle based on Zoeppritz equations. We find that for specific conditions, as the incidence angle increases, the characteristic curve of the transmitted P-wave coefficient enters the third quadrant from the first quadrant through the origin, which produces a transition in the transmitted P wave and the corresponding coefficient experiences polarity reversal. We derive the incidence angle when the transmitted P-wave coefficient is zero and verify that it equals zero by using finite-difference forward modeling for a single-interface model. We replace the water in the model reservoir by gas and see that the reservoir P-wave velocity and density decrease dramatically. By analyzing the synthetic seismogram of the transmitted P wave in the single-interface model, we show that the gas-saturated reservoir is responsible for polarity reversal.展开更多
文摘以多道面波分析技术(MASW)为代表的主动源面波方法已经在地表勘探领域获得越来越多的应用.准确的面波相速度频散成像是利用主动源面波法进行近地表横波速度反演的必要条件.本文提出了一种新的主动源面波频散成像方法—CCPS(Cross-Correlation and Phase-Shifting)法.首先,将单炮面波记录由时空域变换到频率空间域并消去振幅谱的影响,得到归一化频谱.然后,依次将每道信号与整个记录进行互相关的同时进行相速度扫描叠加.最后经过一次求和过程即得到最终的频散图像.通过理论数据、实际工程地震面波资料和石油勘探面波资料比较了普通相移法和CCPS法的频散成像效果.研究表明:新方法相对于普通相移法而言,明显提高了频散图像的质量,相速度聚焦性能和背景噪声压制能力有显著改善.
文摘准确的相速度频散图像是主动源面波勘探方法反演近地表横波速度的基础。提出了一种基于频率-速度域多重信号分类(multiple signal classification in frequency-velocity domain)的面波高分辨率频散成像方法(简称fv-MUSIC方法)。该方法首先将传统的频率-波数域波束形成器改造成频率-速度域形式,然后引入多重信号分类算法将空间谱相关矩阵分解为信号子空间和噪声子空间两个部分,最后利用噪声子空间部分生成最终的面波频散图像。理论数据和实际数据应用结果表明,该方法能产生较高精度的相速度图像,并且使用方便,计算效率高,尤其当接收排列较短时,该方法依然能保持较高的相速度分辨率,有利于提高主动源面波方法的横向速度分辨能力。
基金the National Natural Science Foundation of China(No.41374123)
文摘Polarity reversals may occur to transmitted P waves if the incidence angle is greater than the critical incidence angle. We analyze the characteristics of reflection and transmission coefficients under the condition of wide incidence angle based on Zoeppritz equations. We find that for specific conditions, as the incidence angle increases, the characteristic curve of the transmitted P-wave coefficient enters the third quadrant from the first quadrant through the origin, which produces a transition in the transmitted P wave and the corresponding coefficient experiences polarity reversal. We derive the incidence angle when the transmitted P-wave coefficient is zero and verify that it equals zero by using finite-difference forward modeling for a single-interface model. We replace the water in the model reservoir by gas and see that the reservoir P-wave velocity and density decrease dramatically. By analyzing the synthetic seismogram of the transmitted P wave in the single-interface model, we show that the gas-saturated reservoir is responsible for polarity reversal.
