Compressive sensing seismic acquisition by using regular sampling in an orthogonal grid

Ofelia P. Villarreal, Kareth León, D. Espinosa, W. Agudelo, H. Arguello
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引用次数: 8

Abstract

Seismic survey acquisition permits capturing subsurface data by sensing the seismic waves induced by an artificial source. Hundreds of kilometers are sensed at a sampling rate that satisfies the Nyquist/Shannon theorem to avoid signal aliasing, this means that a high-density arrangement of sensors is required. In seismic, a compressive seismic imaging (CSI) framework has been developed. To test CS theory, random sampling or simultaneous shooting techniques are applied to marine and land environments. For land, random acquisitions require creating new paths on the surface to place each source and receiver, additionally, for terrains with complex access, the artificial used sources are made of dynamite. For this reason, random acquisitions have an elevated environmental impact compared to regular acquisitions, where the same path is used to locate all the sources. This work proposes to use regular sampling (which is not a traditional sampling technique to be used with CS concepts) and to remove sources in a specific configuration present in orthogonal grids with CS concepts in order to reduce acquisition costs and environmental impact. The seismic wave data that should be induced by the removed source is reconstructed using a proposed modified iterative hard thresholding (IHT) algorithm that favors structural similarities of the data. Simulations were performed on real data to illustrate the accuracy of the proposed method, using the Curvelet transformation basis, which attains reconstructions 50% faster than Wavelets.
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基于正交网格规则采样的压缩感知地震采集
地震勘探采集允许通过感应由人工震源引起的地震波来获取地下数据。以满足奈奎斯特/香农定理的采样率检测数百公里,以避免信号混叠,这意味着需要高密度的传感器排列。在地震领域,压缩地震成像(CSI)框架已经被开发出来。为了检验CS理论,随机抽样或同时拍摄技术应用于海洋和陆地环境。对于土地,随机获取需要在地表上创建新的路径来放置每个源和接收器,此外,对于具有复杂通道的地形,使用的人工源由炸药制成。由于这个原因,与常规采集相比,随机采集对环境的影响更大,常规采集使用相同的路径来定位所有来源。这项工作建议使用常规采样(这不是用于CS概念的传统采样技术),并在具有CS概念的正交网格中移除特定配置中的源,以降低获取成本和环境影响。利用改进的迭代硬阈值(IHT)算法,对被移除震源诱发的地震波数据进行重构,该算法有利于数据的结构相似性。在实际数据上进行了仿真,验证了该方法的准确性,该方法采用Curvelet变换基础,重建速度比小波变换快50%。
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