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首页> 外文期刊>Journal of Applied Geophysics >Quality-factor and reflection-coefficient estimation using surface-wave ghost reflections from subvertical structures
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Quality-factor and reflection-coefficient estimation using surface-wave ghost reflections from subvertical structures

机译:利用亚垂直结构面波重影反射进行品质因数和反射系数估算

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摘要

Seismic interferometry can retrieve the Green's function between receivers from the cross-correlation and summation of recordings from a boundary of surrounding sources. Having the sources only along a boundary is sufficient if the medium is lossless. If the medium is dissipative, the retrieved result using cross-correlation contains non-physical (ghost) arrivals. When using receivers at the surface and transient sources in the subsurface for the retrieval of the reflection response in a dissipative medium, it has been shown that the retrieved ghost reflections are characteristic of the quality factor of the subsurface. The ghost reflections are caused by internal reflections inside subsurface layers. It has been shown with numerical examples for recordings in a borehole from a surface source that a ghost reflection can be discriminated from physical reflections and tied to a specific subsurface layer. After connecting the ghost reflection to a specific layer, the quality factor of the medium above this layer and the reflection coefficient at the layer interface can be estimated. In this article, we show how the above principles can be adapted and applied for surface waves. Due to intrinsic losses in the medium, surface-wave ghost reflections are retrieved from internal scattering between subvertical boundaries. We demonstrate the method on an ultrasonic dataset recorded on a sample composed of a PVC block and an aluminum block. The aluminum block has a groove parallel to the PVC/aluminum interface. Using a surface-wave ghost reflection between the groove and the PVC/aluminum interface, we estimate the quality factor of the PVC and the reflection coefficient at the PVC/aluminum interface. We also show that the ghost reflection can be identified and tied to the layer between the groove and the PVC/aluminum interface, thus confirming previous numerical findings. (C) 2014 Elsevier B.V. All rights reserved.
机译:地震干涉法可以根据互相关和周围源边界的记录求和求出接收机之间的格林函数。如果介质是无损的,仅沿边界放置源就足够了。如果介质具有耗散性,则使用互相关的检索结果将包含非物理(虚假)到达。当使用地表下的接收器和地下的瞬变源来获取耗散介质中的反射响应时,已表明,所获取的重影反射是地下质量因数的特征。重影反射是由地下层内部的内部反射引起的。已经用数字示例示出了从地面源在井眼中进行记录的情况,重影反射可以与物理反射区分开并绑定到特定的地下层。将重影反射连接到特定层后,可以估算该层上方介质的品质因数和层界面处的反射系数。在本文中,我们展示了如何将上述原理应用于表面波。由于介质中的固有损耗,因此从垂直下边界之间的内部散射中获取了表面波重影反射。我们在记录由PVC块和铝块组成的样品上的超声数据集上演示了该方法。铝块具有平行于PVC /铝界面的凹槽。使用凹槽和PVC /铝界面之间的表面波幻影反射,我们估算了PVC的品质因数以及PVC /铝界面的反射系数。我们还表明,可以识别出幻影反射并将其绑定到凹槽与PVC /铝界面之间的层,从而证实了先前的数值发现。 (C)2014 Elsevier B.V.保留所有权利。

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