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P-Wave Reflection Imaging

机译:P波反射成像

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The reflection of elastic waves from interfaces is a robust phenomenon extensively used by animals (bats and dolphins), nondestructive techniques, and medical diagnosis. This study addresses the design and implementation of P-wave reflection imaging to evaluate the internal variability in small-scale submerged, soil models. The performance of this technology depends on fundamental aspects of P-wave propagation in soils, the selection of optimal P-wave transducers, and the development of an adequate test methodology. Design issues include transducer directivity, noise, axial resolution, near field effects, and proper thickness of the coupling water layer. The operating frequency is determined by transducer selection and affects the axial and lateral resolution, skin depth, near field, and divergence; high damping transducers permit higher axial resolution. In addition, data gathering must take into consideration temporal and spatial aliasing. Results show that P-wave reflection is a valuable tool to detect subsurface anomalies and layers, to assess phenomena such as slurry sedimentation, and to monitor the evolution of subsurface structures such as soil layers during liquefaction. Gradual changes in impedance, such as in slurry sedimentation, may prevent reflections.
机译:来自界面的弹性波反射是一种坚固的现象,已被动物(蝙蝠和海豚),无损技术和医学诊断广泛使用。这项研究致力于P波反射成像的设计和实现,以评估小规模水下土壤模型的内部变异性。该技术的性能取决于土壤中P波传播的基本方面,最佳P波换能器的选择以及适当测试方法的发展。设计问题包括换能器方向性,噪声,轴向分辨率,近场效应以及耦合水层的适当厚度。工作频率取决于换能器的选择,并且会影响轴向和横向分辨率,趋肤深度,近场和发散度;高阻尼传感器可实现更高的轴向分辨率。另外,数据收集必须考虑时间和空间混叠。结果表明,P波反射是检测地下异常和层,评估泥浆沉降等现象以及监测液化过程中地下结构(如土壤层)演变的宝贵工具。阻抗的逐渐变化(例如泥浆沉淀)可以防止反射。

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