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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Estimation of elastic stiffness coefficients of an orthorhombic physical model using group velocity analysis on transmission data
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Estimation of elastic stiffness coefficients of an orthorhombic physical model using group velocity analysis on transmission data

机译:基于群速度分析的正交各向异性物理模型弹性刚度系数估算

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摘要

We acquired 3C ultrasonic transmission seismograms, measured group velocities associated with the three quasi-body wave types, and determined density-normalized stiffness coefficients (A_ij = C_ij∕ρ) over an orthorhombic physical (laboratory) model. The estimation of A_ij is based on an approximate relationship between the nine orthorhombic A_ij and group velocities. Estimation of the anisotropic A_ij is usually done using phase velocities with well-known formulas expressing their theoretical dependence on A_ij. However, on time-domain seismograms, arrivals are observed traveling with group velocities. Group velocity measurements are found to be straightforward, reasonably accurate, and independent of the size of the transducers used. In contrast, the accuracy of phase velocities derived from the eτ; pT transform analysis was found to be very sensitive to small differences in picked arrival times and to transducer size. Theoretical phase and group velocities, calculated in a forward manner from the A_ij estimates, agreed with the originally measured phase and group velocities, respectively. This agreement confirms that it is valid to use easily measured group velocities with their approximate theoretical relationship to the A_ij to determine the full stiffness matrix. Compared to the phase-velocity procedure, the technique involving group velocities is much less prone to error due to time-picking uncertainties, and therefore is more suitable for analyzing physical model seismic data.
机译:我们获得了3C超声传输地震图,测量了与三种准体波类型相关的群速度,并确定了正交正交物理(实验室)模型的密度归一化刚度系数(A_ij = C_ij ∕ρ)。 A_ij的估计基于九个正交A_ij与群速度之间的近似关系。各向异性A_ij的估算通常是使用相速度完成的,该相速度采用众所周知的公式表示其对A_ij的理论依赖性。但是,在时域地震图中,观测到的到达以群速度传播。组速度测量被发现是简单,合理,准确的,并且与所使用的换能器的尺寸无关。相反,从eτ推导出相速度的精度;发现pT变换分析对拾取的到达时间的微小差异和传感器尺寸非常敏感。从A_ij估计值向前计算得出的理论相速度和组速度分别与最初测量的相速度和组速度一致。该协议确认使用易于测量的群速度及其与A_ij的近似理论关系来确定整个刚度矩阵是有效的。与相速度程序相比,涉及群速度的技术由于时间选择的不确定性而更容易出错,因此更适合于分析物理模型地震数据。

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