干湿循环对各种风化级砂岩微观结构的影响

K. S. Shah, Mohd Hazizan bin Mohd Hashim, H. Rehman, K. S. Ariffin
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引用次数: 0

摘要

本研究调查了岩石与水的相互作用对各种风化级砂岩微观结构特性的影响。砂岩样本取自巴基斯坦 Sor-Range 煤矿区,并使用台式扫描电子显微镜(SEM)进行了研究。使用 ImageJ 软件从显微照片中获得了微观结构的特征。研究结果表明,干湿循环的增加对微观结构(孔隙和微裂缝)有明显影响。砂岩的孔隙率和微裂缝密度随着干湿循环次数的增加而增加。此外,随着风化等级的增加,微裂缝的长度也会增加。由于岩石宏观力学特征的变化与微观结构的恶化直接相关。因此,分析不同风化等级岩石中水-岩相互作用的影响,可为评估岩土结构的稳定性提供更准确的参考指标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effect of Wet-Dry Cycling on the Microstructure of Various Weathering Grade Sandstone
This study investigated the effect of rock-water interaction on microstructural properties of various weathering grade sandstone. Sandstone samples were acquired from the Sor-Range coal mine area, Pakistan, and were investigated using a tabletop scanning electron microscope (SEM). The characteristics of microstructures from micrographs were obtained using ImageJ software. According to the findings an increase in wet and dry cycles significantly affects the microstructures (pore spaces and microcracks). The porosity and microcracks density of sandstone increases with the number of wet and dry cycles. Furthermore, the length of microcracks increases as the weathering grade increases. As variation in rock macroscopic mechanical characteristics is directly associated with the deterioration of microstructures. Therefore, analyzing the effect of water-rock interaction in various weathering grades of rock can offer a more accurate reference index for assessing the stability of geotechnical structures.
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