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Flux-normalized Elastodynamic Wavefield Decomposition using only Particle Velocity Recordings

机译:仅使用粒子速度记录的磁通归一化弹性动力波面分解

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We present a new approach to apply wavefield decomposition, illustrated for an energy flux-normalized elastodynamic case. We start by considering a situation where two horizontal boreholes are closely separated from each other. By recording only the particle velocities at both depth levels (for example with conventional 3-component geophones) and expressing the one-way wavefields at one depth level in terms of the fields at the other depth level, an inverse problem can be formulated and solved. This new approach of multi-depth level (MDL) wavefield decomposition is illustrated with a synthetic 2D finite-difference example, showing correct one-way wave-field retrieval. We then modify the methodology for a special case with a single receiver array just below a free surface, where the problem is naturally constrained by the (Dirichlet) boundary condition at the free-surface. Again, it is shown that correct elastodynamic wavefield decomposition takes place, for both P- and S-waves.
机译:我们提出了一种应用波场分解的新方法,用于能量通量归一化弹性动力学情况。我们首先考虑到两个水平钻孔彼此紧密分离的情况。通过仅记录两个深度水平的粒子速度(例如,与传统的3组件地震检到)并在另一个深度水平处的字段的一个深度级别表示单向波场,可以制定和解决逆问题。使用合成2D有限差示例示出了这种多深度(MDL)波场分解的新方法,显示了正确的单向波场检索。然后,我们用一个特殊情况修改特殊情况的方法,其中单个接收器阵列在自由表面下方,其中问题自由表面处的(Dirichlet)边界条件自然地限制。同样,示出了对于P和S波来说,发生了正确的弹性动力波面分解。

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