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Estimation of Fracture Toughness of Anisotropic Rocks by Semi-Circular Bend (SCB) Tests Under Water Vapor Pressure

机译:水蒸气压力下半圆弯曲(SCB)试验估算各向异性岩石的断裂韧性

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In order to investigate the influence of water vapor pressure in the surrounding environment on mode I fracture toughness (K-Ic) of rocks, semi-circular bend (SCB) tests under various water vapor pressures were conducted. Water vapor is one of the most effective agents which promote stress corrosion of rocks. The range of water vapor pressure used was 10(-2) to 10(3) Pa, and two anisotropic rock types, African granodiorite and Korean granite, were used in this work. The measurement of elastic wave velocity and observation of thin sections of these rocks were performed to investigate the microstructures of the rocks. It was found that the distribution of inherent microcracks and grains have a preferred orientation. Two types of specimens in different orientations, namely Type-1 and Type-3, were prepared based on the anisotropy identified by the differences in the elastic wave velocity. K-Ic of both rock types was dependent on the water vapor pressure in the surrounding environment and decreased with increasing water vapor pressure. It was found that the degree of the dependence is influenced by the orientation and density of inherent microcracks. The experimental results also showed that K-Ic depended on the material anisotropy. A fracture process was discussed on the basis of the geometry of fractures within fractured specimens visualized by the X-ray computed tomography (CT) method. It was concluded that the dominant factor causing the anisotropy of K-Ic is the distribution of grains rather than inherent microcracks in these rocks.
机译:为了研究周围环境中水蒸气压力对岩石I型断裂韧度(K-Ic)的影响,在各种水蒸气压力下进行了半圆弯曲(SCB)试验。水蒸气是促进岩石应力腐蚀的最有效的物质之一。所使用的水蒸气压力范围为10(-2)至10(3)Pa,并且在这项工作中使用了两种各向异性的岩石类型:非洲花岗闪长岩和韩国花岗石。进行了弹性波速度的测量和这些岩石的薄层的观察,以研究岩石的微观结构。发现固有的微裂纹和晶粒的分布具有优选的取向。根据由弹性波速度的差异确定的各向异性,制备了两种类型的不同方向的标本,即Type-1和Type-3。两种岩石的K-Ic都取决于周围环境中的水蒸气压力,并且随着水蒸气压力的增加而降低。已经发现,依赖程度受固有微裂纹的取向和密度影响。实验结果还表明,K-Ic取决于材料的各向异性。根据X射线计算机断层扫描(CT)方法可视化的断裂标本中的断裂几何形状,讨论了断裂过程。可以得出结论,引起K-Ic各向异性的主要因素是这些岩石中晶粒的分布,而不是固有的微裂纹。

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