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Influence of relative humidity on fracture toughness of rock: implications for subcritical crack growth

机译:相对湿度对岩石断裂韧度的影响:对亚临界裂纹扩展的影响

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摘要

Information relating to the fracture toughness of geomaterials is critical to our understanding of tensile fracturing, and in particular in geological and rock engineering projects that are subjected to elevated moisture levels. In this study, we conducted a comprehensive set of fracture toughness tests on a suite of key rock types in air under different relative humidities and at constant temperature in order to investigate the influence of relative humidity on fracture toughness. Three sandstones and two igneous rocks were chosen for this purpose. We show that the value of fracture toughness decreases with increasing relative humidity. In addition, we find that the decrease in fracture toughness was more significant when the expansive clay such as smectite was included in rock. Since smectite is prone to expanding in the presence of water, the strength and thus crack growth resistance decrease when relative humidity is high. Therefore, we interpret the decreasing fracture toughness upon the degradation of expansive clays with increasing water content. It was also shown that the decrease of the fracture toughness with increasing humidity is less significant than the concomitant decrease in the measured value of the subcritical stress intensity factor. This was likely as a result of stress corrosion having little influence on the fracture toughness. We conclude that crack growth in rock is affected by humidity, and that clay content is an important contributing factor to changes in fracture toughness and subcritical stress intensity factor.
机译:与土工材料的断裂韧性有关的信息对于我们对拉伸断裂的理解至关重要,特别是在水分含量较高的地质和岩石工程项目中。在这项研究中,我们对一组在不同相对湿度和恒定温度下的空气中的关键岩石类型进行了一套全面的断裂韧性测试,以研究相对湿度对断裂韧性的影响。为此选择了三个砂岩和两个火成岩。我们表明,断裂韧性的值随着相对湿度的增加而降低。另外,我们发现,当岩石中包括蒙脱石等膨胀粘土时,断裂韧性的降低更为显着。由于蒙脱石在水的存在下易于膨胀,因此当相对湿度高时,强度和因此抗裂纹扩展性降低。因此,我们解释了随着含水量的增加,膨胀黏土的降解会降低断裂韧性。还显示出,随着湿度的增加,断裂韧性的降低不如伴随的亚临界应力强度因子的测量值的降低显着。这可能是由于应力腐蚀对断裂韧性影响很小的结果。我们得出的结论是,岩石的裂纹扩展受湿度影响,并且粘土含量是导致断裂韧性和亚临界应力强度因子变化的重要因素。

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