Investigation of three-dimensional model reconstruction and fractal characteristics of crack propagation in jointed sandstone

IF 3.9 2区 工程技术 Q3 ENERGY & FUELS Geomechanics and Geophysics for Geo-Energy and Geo-Resources Pub Date : 2024-04-20 DOI:10.1007/s40948-024-00797-3
Ziqi Liu, Lulin Zheng, Yujun Zuo, Hao Liu, Yuanjiang Hou, Zehua Zhu, Zhibin Hao, Xiaokun Wang, Gang Huang
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Abstract

The presence of random joints, cracks, and other defects significantly affects the meso-damage mechanism and macro-mechanical behavior of the rock. This study employed micro-CT scanning, digital image processing (DIP), and the rock failure process analysis system (RFPA3D) to reconstruct a genuine mesostructure, creating a three-dimensional (3D) numerical model of jointed sandstone. Under uniaxial stress, this model facilitated the meso-damage evolution process of prefabricated cracks in sandstone with varying dip angles. Additionally, the influence of jointed sandstone heterogeneity and prefabricated cracks with various dip angles on its failure mode and meso-damage mechanical properties were investigated. Utilizing the MATLAB platform, a 3D box dimension algorithm was developed to analyze the fractal characteristics of the mesodamage evolution in the sample. This algorithm enabled the quantitative characterization of the meso-damage evolution of sandstone. This study categorized three types of sandstone final failure modes: composite shear failure, shear failure along the joint surface, and tensile failure. Additionally, linear variations in the elastic modulus and compressive strength of the jointed sandstone were observed with increasing prefabricated fracture inclination, highlighting significant anisotropy. The presence of joints was found to induce and control the failure mode of sandstone. The meso-damage evolution process of sandstone was described in terms of the fractal dimension, indicating that more severe damage corresponded to a larger fractal dimension. This approach offers a novel statistical method for studying the progression of rock damage.

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节理砂岩裂纹扩展的三维模型重建和分形特征研究
随机节理、裂缝和其他缺陷的存在会严重影响岩石的中观破坏机制和宏观力学行为。本研究采用显微 CT 扫描、数字图像处理(DIP)和岩石破坏过程分析系统(RFPA3D)重建了真实的中观结构,创建了节理砂岩的三维(3D)数值模型。在单轴应力作用下,该模型有助于研究不同倾角砂岩中预制裂缝的中观破坏演化过程。此外,还研究了节理砂岩异质性和不同倾角的预制裂缝对其破坏模式和介观破坏力学性能的影响。利用 MATLAB 平台,开发了一种三维盒尺寸算法,用于分析样品中层损伤演变的分形特征。该算法可定量分析砂岩的中观损伤演变特征。该研究将砂岩的最终破坏模式分为三种:复合剪切破坏、沿接合面的剪切破坏和拉伸破坏。此外,随着预制断裂倾角的增加,节理砂岩的弹性模量和抗压强度也出现了线性变化,凸显了显著的各向异性。研究发现,接缝的存在诱发并控制了砂岩的破坏模式。用分形维度描述了砂岩的中观损伤演变过程,表明损伤越严重,分形维度越大。这种方法为研究岩石损伤的进展提供了一种新的统计方法。
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来源期刊
Geomechanics and Geophysics for Geo-Energy and Geo-Resources
Geomechanics and Geophysics for Geo-Energy and Geo-Resources Earth and Planetary Sciences-Geophysics
CiteScore
6.40
自引率
16.00%
发文量
163
期刊介绍: This journal offers original research, new developments, and case studies in geomechanics and geophysics, focused on energy and resources in Earth’s subsurface. Covers theory, experimental results, numerical methods, modeling, engineering, technology and more.
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