粗颗粒砂砾岩内矿物颗粒和孔隙结构的非均匀性及量化表征细观试验研究

Microscopic experimental study on the heterogeneity and quantitative characterization of mineral grains and pore structures in coarse-grained glutenites

  • 摘要: 岩石的非均匀性是导致其在外力作用下宏观力学性能呈现非线性的本质原因。为了研究矿物颗粒和孔隙结构对岩石非均匀性影响程度的大小,以粗颗粒砂砾岩为研究对象进行CT扫描试验,运用三维重构技术和图像阈值分割技术,三维重构矿物颗粒和孔隙结构,量化表征矿物颗粒和孔隙结构的特征,通过统计学的方法,分析粗颗粒砂砾岩的非均匀特性,构建岩石的非均匀性综合指数,探讨影响岩石非均匀性的关键因素。研究结果表明,孔隙形状、孔隙直径和孔隙度可以表征孔隙结构的非均匀性,孔隙直径是影响孔隙结构非均匀性的关键因素,孔隙度是影响孔隙结构非均匀性的次要因素,孔隙形状是影响孔隙结构非均匀性的非关键因素;矿物形状、矿物粒径和矿物颗粒体积分数可以表征矿物颗粒的非均匀性,矿物颗粒体积分数是影响矿物颗粒非均匀性的关键因素,矿物粒径是影响矿物颗粒非均匀性的次要因素,矿物形状是影响矿物颗粒非均匀性的非关键因素。岩石非均匀性的综合指数与矿物颗粒的非均匀性系数变化规律一致,岩石的非均匀性主要由矿物颗粒的非均匀性决定,矿物颗粒体积分数是影响岩石非均匀性的核心因素,矿物形状是影响岩石非均匀性的最小因素。量化表征岩石内矿物颗粒和孔隙结构的非均匀性可以对岩石的整体性能和稳定性进行更准确的评估,可用于预测岩体工程中存在的潜在风险,从而采取相应的预防措施,确保工程的安全和稳定。

     

    Abstract: The heterogeneity of rock is the essential reason for its nonlinear macroscopic mechanical properties under external forces. To study the degree of influence of mineral particles and pore structure on the heterogeneity of rock, coarse-grained glutenites were subjected to CT scanning. The three-dimensional reconstruction technology and image threshold segmentation technology were used to reconstruct the mineral particles and pore structure. The characteristics of mineral particles and pore structures were quantified. The heterogeneity characteristics of coarse-grained glutenites were analyzed through statistical methods. A comprehensive index of rock heterogeneity was constructed to explore the key factors affecting rock heterogeneity. The results show that pore shape, pore diameter, and porosity can characterize the heterogeneity of the pore structure, where pore diameter is the key factor affecting the heterogeneity of the pore structure, porosity is a secondary factor, and pore shape is a non-critical factor; Mineral shape, mineral diameter, and the volume fraction of mineral particles can characterize the heterogeneity of mineral particles. The volume fraction of mineral particles is the key factor affecting the heterogeneity of mineral particles, mineral diameter is a secondary factor, and mineral shape is a non-critical factor. The comprehensive index of rock heterogeneity is consistent with the variation pattern of the mineral particle heterogeneity coefficient. The heterogeneity of rock is mainly determined by the heterogeneity of mineral particles, with the volume fraction of mineral particles being the core factor affecting rock heterogeneity, and mineral shape being the least influential factor. Quantifying the heterogeneity of mineral particles and pore structure inside the rock can more accurately assess the overall performance and stability of the rock. It can be used to predict potential risks in rock engineering and adopt corresponding preventive measures to ensure the safety and stability of the projects.

     

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