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首页> 外文期刊>International Journal of Rock Mechanics and Mining Sciences >Effects of local rock heterogeneities on the hydromechanics of fractured rocks using a digital-image-based technique
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Effects of local rock heterogeneities on the hydromechanics of fractured rocks using a digital-image-based technique

机译:基于数字图像技术的局部岩石非均质性对裂隙岩石流体力学的影响

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摘要

A digital-image-based (DIB) finite element approach is developed based on the numerical code rock failure process analysis (RFPA) to characterize micro-scale rock heterogeneity, and to understand the impact of micro-scale rock heterogeneity on the macro-scale hydromechanical response of rocks. The DIB technique incorporates small-scale spatial variability of initial deformation modulus, strength and permeability directly into a coupled hydromechanical model. Variability in Young's modulus, strength, and permeability is applied by a property map defined from the pixel-scale of a digital image. In the RFPA, mechanical deformation is followed, including the accumulation of damage applied in individual elements, which modifies modulus, strength, and permeability with the intensity of damage. The RFPA simulates progressive failure in fractured rocks, representing both the growth of existing fractures and the formation of new fractures, without having to identify crack tips and their interaction explicitly. In this DIB simulation approach, image voxels are used to give equivalent mechanical and flow properties. These property maps are ported to the model capable of solving directly for the evolving deformation, and fluid flow fields. The model is validated through comparisons of the simulated results with phenomenological observations documented in previous studies. The validated model is then applied to investigate the hydromechanical response of fractured rock characterized by digital image. The model is able to reproduce the spatial evolution of damage in the sample, the coalescence of existing cracks, and the formation of new cracks.
机译:基于数值岩石破坏过程分析(RFPA),开发了一种基于数字图像的(DIB)有限元方法,以表征微观岩石非均质性,并了解微观岩石非均质性对宏观尺度的影响。岩石的流体力学响应。 DIB技术将初始变形模量,强度和渗透率的小范围空间变异性直接纳入耦合的水力模型中。杨氏模量,强度和磁导率的变化是通过从数字图像的像素比例定义的特性图得出的。在RFPA中,会进行机械变形,包括在各个元素中施加的损伤累积,从而随损伤强度修改模量,强度和磁导率。 RFPA可以模拟裂隙岩石的渐进破坏,既代表现有裂缝的增长,又代表新裂缝的形成,而不必明确识别裂纹尖端及其相互作用。在这种DIB仿真方法中,图像体素用于提供等效的机械和流动特性。将这些特性图移植到能够直接求解不断演变的变形和流体流场的模型。通过将模拟结果与先前研究中记录的现象学观察结果进行比较来验证该模型。然后将经过验证的模型应用于研究以数字图像表征的裂隙岩体的水力响应。该模型能够再现样品中损伤的空间演化,现有裂纹的合并以及新裂纹的形成。

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