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Tomographic Imaging of Thermally Induced Fractures in Granite Using Bayesian Inversion

机译:利用贝叶斯反演对花岗岩中热致断裂的层析成像

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— The internal structure of rock samples studied in laboratory experiments can be described by a variety of physical parameters. Some of them, like the velocity of acoustic waves, enhanced velocity or quality factor can be reconstructed by means of ultrasonic tomography. This article presents the results of classical velocity tomography imaging, accompanied by the results of attenuation tomography and recently introduced enhanced velocity tomography obtained for a Lac Du Bonnet granite sample subjected to thermal stresses. To invert acoustic data recorded during six heating cycles, a Bayesian inversion scheme accompanied by a genetic algorithm optimization approach and the robust Cauchy norm have been used. To obtain the highest possible spatial resolution of images the inversion was performed in two steps. In the first step a crude parameterization of the sample was used. The result of this stage was next taken as an a priori model for a final inversion with refined parameterization. The choice of parameterization (cell sizes) and damping parameters at both stages was based on an analysis of the resolution operator. Both velocity and enhanced velocity tomography accurately imaged changes in the rock microstructure caused by thermal stresses. However, enhanced velocity tomography gave a much better spatial resolution than velocity tomography. On the other hand, attenuation tomography based on inversion of pulse rise times was able to image only a rough structure of the sample and it has difficulty with reasonable imaging of the crack formed in the sixth heating cycle.
机译:—在实验室实验中研究的岩石样品的内部结构可以通过多种物理参数来描述。它们中的一些,例如声波的速度,增强的速度或品质因数,可以通过超声层析成像来重建。本文介绍了经典速度层析成像的结果,以及衰减层析成像的结果,以及最近介绍的Lac Du Bonnet花岗岩样品在热应力作用下获得的增强速度层析成像。为了对六个加热周期中记录的声学数据进行反演,已经使用了贝叶斯反演方案以及遗传算法优化方法和鲁棒的柯西范数。为了获得图像的最高空间分辨率,反演分两个步骤进行。第一步,使用样品的粗略参数化。接下来,将这一阶段的结果作为先验模型进行最终的反演,并进行精确的参数化。在两个阶段中对参数化(像元大小)和阻尼参数的选择均基于对分辨率算符的分析。速度层析成像和增强速度层析成像都可以准确地成像由热应力引起的岩石微观结构变化。但是,增强的速度层析成像技术比速度层析成像技术具有更好的空间分辨率。另一方面,基于脉冲上升时间倒置的衰减层析成像仅能对样品的粗糙结构成像,并且难以合理地成像在第六加热循环中形成的裂纹。

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