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Evaluation of Subsurface Structure at Soultz Hot Dry Rock Site by the AE Reflection Method in Time-frequency Domain

机译:时频域AE反射法评价Soultz热干岩场地地下结构

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摘要

Because the Soultz Hot Dry Rock (HDR) site, France, is to be expanded to a scientific pilot plant of greater depth, measurement of the deep area below the predeveloped artificial reservoir is gaining importance. In this paper, we present estimates of deep subsurface structure at the Soultz HDR site, obtained by a reflection method using acoustic emission (AE) signals, that is, induced seismicity, as the wave source. First, we briefly describe the AE reflection method in the time-frequency domain with wavelet transform. Then we show estimates of the subsurface structure by using 101 high-energy AE events observed in 1993. We compare and discuss the results obtained, using the AE reflection method in two wells with other independent borehole observations. Furthermore, we present the results of an investigation of the frequency dependence of reflectors identified by hodogram linearity as a possible means of further characterizing detected structures.
机译:由于法国的Soultz热干岩(HDR)站点将扩展到更大深度的科学试点工厂,因此对预先开发的人工油藏下方的深层区域进行测量变得越来越重要。在本文中,我们介绍了Soultz HDR站点的深层地下结构的估计,该估计是通过使用声发射(AE)信号(即感应地震)作为波源的反射方法获得的。首先,我们简要描述小波变换在时频域中的声发射反射方法。然后,我们使用1993年观测到的101个高能声发射事件显示了地下结构的估计。我们在两个井中使用声发射反射方法以及其他独立的井眼观测结果,对所得结果进行了比较和讨论。此外,我们提出了对由反射图线性确定的反射器的频率依赖性进行研究的结果,作为进一步表征检测到的结构的可能手段。

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