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首页> 外文期刊>IEEE Transactions on Ultrasonics, Ferroelectrics, and Frequency Control >Finite-Element Analysis of Noise Preceding the Arrival of S-Wave in Ultrasonic Measurements of Rock Velocities
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Finite-Element Analysis of Noise Preceding the Arrival of S-Wave in Ultrasonic Measurements of Rock Velocities

机译:岩石速度超声测量中S波噪声的有限元分析

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For oil and gas seismic exploration, rock velocities are essential parameters to tease out reservoir properties from seismic data. The ultrasonic pulse transmission (UPT) method has been a gold standard to estimate reservoir rock velocities in the laboratory. Regarding the UPT method, accurate determination of the travel time of waves plays a significant role in robustly measuring rock velocities. One of the most conventional ways to obtain the travel time is through the arrival picking. However, unclear noise virtually exists preceding the arrival of S-wave interfering with this arrival picking, which, sometimes, can cause enormous errors to measured S-wave velocity. Herein, we develop a 2-D, three-component (2D-3C) finite-element modeling (FEM) algorithm aiming to interpret the noise by combining with UPT measurements. The proposed 2D-3C FEM not only can efficiently compute ultrasonic wavefield radiated by circular P- or S-wave transducers but also able to obtain synthetic waveforms in the testing of S-wave velocity where polarization directions of S-wave transducers are arranged as nonparallel. To analyze the simulated ultrasonic waveforms, we introduce frequently-used concepts of edge and direct plane waves to build elastodynamic models of the ultrasonic wavefield. Then, we compare numerical results with experimental measurements. Our 2D-3C FEM results show good agreement with experimental waveforms both in P- and S-wave velocity testings. Whereafter, we pinpoint constitutions of the noise preceding the arrival of S-wave. Comparison of numerical and experimental waveforms suggests that the edge P-wave with its reflected and converted modes partially contributes to this noise, while the rest part of the noise may stem from the effects of the compressional dipole, the couplant smeared between a transducer and a sample, and inherently parasitic longitudinal vibrations of S-wave transducers. The interpretations on this noise have the potential to benefit future design of more effective S-wave transducers.
机译:对于石油和天然气地震勘探,岩石速度是梳理地震数据的储层性质的基本参数。超声波脉冲传输(UPT)方法是黄金标准,以估算实验室中的储层岩石速度。关于UPT方法,准确地确定波浪的行程时间在鲁棒地测量岩石速度中起着重要作用。获得旅行时间的最传统方式之一是通过到达挑选。然而,在S波干扰的到来之前,几乎存在的噪声几乎存在,有时会导致测量的S波速度造成巨大误差。这里,我们开发了一种二进制,三分组分(2D-3C)有限元建模(FEM)算法,其旨在通过与UPT测量组合来解释噪声。所提出的2D-3C FEM不仅可以有效地计算由圆形P型或S波换能器辐射的超声波波场,而且还能够在测试S波速度的测试中获得合成波形,其中S波换能器的偏振方向被布置为非平行。为了分析模拟的超声波波形,我们引入了常用的边缘和直平面波的概念,以构建超声波波场的弹性动力学模型。然后,我们将数值结果与实验测量进行比较。我们的2D-3C FEM结果与P-和S波速度测试中的实验波形均匀吻合。然后,我们针对S波到来之前的噪声定位施工。数值和实验波形的比较表明,具有其反射和转换模式的边缘P波部分地有助于这种噪音,而噪声的静止部分可以源于压缩偶极子的效果,耦合器之间涂抹在换能器之间的效果。样品,以及固有的S波换能器的寄生纵振振动。对这种噪声的解释有可能使未来设计更有效的S波传感器的可能性。

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