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3D imaging of fractures in carbonate rocks using X-ray computed tomography technology

机译:使用X射线计算机断层扫描技术对碳酸盐岩裂缝进行3D成像

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摘要

A number of techniques have been developed to detect and study fractures growth in rocks in the past few decades. Among them, the high-resolution X-ray computed tomography (CT) is a useful, rapid and nondestructive way to test and visualize the interiors of rocks in two and three dimensions. The difference in X-ray absorption between the mineral grains and the fractures can create well-contrasted CT images. In this paper, the main objective is to image the fractures in carbonated rock under uniaxial compression and rock fracturing experiments using the CT imaging technique in three dimensions. In the uniaxial compression test, the CT technology is performed to observe the macroscopic fractures in rock after failure. The 3D tomograms indicate that microcracks in rock mutually interconnect and eventually form macroscopic fractures. Then, the rock fracturing experiment is conducted to observe the geometry of induced fractures with the aid of the CT imaging. The 3D tomograms and visualized images show that the induced fracture intersects with the surface of rock sample, indicating that the CT technology can depict the induced fracture accurately. Moreover, the 3D visualized images illustrate that the macroscopic induced fracture in rock is produced with well-developed roughness. The experimental results show that the CT technique is a useful way to observe the fractures in rocks.
机译:在过去的几十年中,已经开发出许多技术来检测和研究岩石中的裂缝增长。其中,高分辨率X射线计算机断层扫描(CT)是一种有用,快速且无损的测试和可视化岩石内部和二维空间的方法。矿物颗粒和裂缝之间的X射线吸收差异会产生对比度良好的CT图像。本文的主要目的是利用CT成像技术在三维上对碳酸盐岩的单轴压缩和岩石破裂实验中的裂缝进行成像。在单轴压缩试验中,使用CT技术观察破裂后岩石的宏观裂缝。 3D断层图表明,岩石中的微裂纹相互连接,最终形成宏观裂缝。然后,进行岩石压裂实验,借助CT成像观察诱导裂缝的几何形状。 3D断层图和可视化图像显示,诱导裂缝与岩石样品表面相交,这表明CT技术可以准确地描绘诱导裂缝。此外,3D可视化图像表明,岩石中的宏观诱发裂缝产生的粗糙度很好。实验结果表明,CT技术是观察岩石裂缝的有效方法。

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