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Integration of rock images and laboratory data through the lens of a new discipline

机译:通过新纪律的镜头整合岩石图像和实验室数据

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This paper represents an effort to outline some issues and potential guidelines associated with the integration of rock images with laboratory data. It is entirely based on the use of X-ray computed tomography (CT) imaging, which has become more readily accessible over the years and allows for non-destructively imaging geomaterials in three dimensions over many length scales (~10-9 to 100 m). While the number of studies involving X-ray CT scanning has been steadily growing, there is a paucity of rules regarding the conduct of that imaging work compared to the well established set of protocols that exist around all aspects of experimental geomechanics. To correct for this imbalance and build a common experience within the community, the identification of image and lab data integration as a discipline could be of tremendous help as it would allow to devise principles and focus efforts on areas most in need of improvement. More importantly, this new discipline would naturally take on the role of building image-based predictive petrophysical and geomechanical models by leveraging many decades of research on the microstructural control of physical properties. Such image-based modeling effort would require to shift the role of high performance computing tools from simulation to description, with two immediate advantages: (1) A very efficient predictive capability compared to numerical simulations (through constitutive laws) and (2) The associated benefit of phenomenological understanding.
机译:本文代表了概述与实验室数据集成相关的一些问题和潜在指导方针。它完全基于X射线计算断层扫描(CT)成像的使用,这在多年上变得更加容易访问,并且允许在许多长度范围内(〜10-9至100米)三维非破坏性成像地质材料(〜10-9 )。虽然涉及X射线CT扫描的研究数量稳定地增长,但是与在实验性地质力学的各个方面周围的所有方面存在的良好成熟的协议相比,缺乏关于该影像作用的行为的规则。为纠正这种不平衡并在社区内建立共同的经验,作为一个学科的形象和实验室数据集成的识别可能是巨大的帮助,因为它可以使原则设计和焦点在最需要改进的区域上进行努力。更重要的是,这种新的学科自然会通过利用数十年来建立基于图像的预测岩石物理和地质力学模型的作用对物理性质的微观结构控制的几十年来。这种基于图像的建模努力将需要将高性能计算工具的角色从模拟转移到描述,具有两个即时的优势:(1)与数值模拟(通过本构规则)和(2)相关的相比非常有效的预测能力现象理解的好处。

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