单轴压缩作用下沉积岩的力学与断裂行为

K. Ng, Esra’a Alomari, Lokendra Khatri
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摘要

与能量相关的表征可以提供有关岩石力学行为的重要信息。对美国怀俄明州的完整岩样进行了一系列单轴压缩试验。首先检查了样品的物理性质(即孔隙率和晶粒尺寸)。为了研究沉积岩的断裂行为,利用已发表的数据集汇编和我们的实验数据,开发了一种基于岩石变形过程中释放的能量(即岩石韧性)估计单轴抗压强度(UCS)的新方法。能量释放计算为应力-应变曲线下直至达到峰值应力的面积。这种能量与岩石的密度密切相关。在此基础上,提出了一种基于岩石韧性的预测经验模型。通过对比试验岩石抗压强度的预测值和实测值,验证了该经验模型的有效性,其平均偏差(实测抗压强度与预测抗压强度之比)为1.002。
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Mechanical and Fracture Behavior of Sedimentary Rocks under Uniaxial Compression
Energy-related characterizations can provide important information regarding mechanical behavior of rocks. A series of uniaxial compression tests were carried out on intact rock samples obtained from Wyoming, USA. The physical properties of the samples (i.e., porosity and grain size) were first examined. To investigate the fracture behavior of sedimentary rocks, a compilation of published dataset and our experimental data were employed to develop a new approach for estimating uniaxial compressive strength (UCS) based on the amount of energy released during rock deformation, which is known as the rock toughness. The energy release is calculated as the area under the stress-strain curve until the peak stress is reached. This energy shows a strong correlation with the density of the rock. Moreover, a predictive empirical model was proposed to estimate the rock UCS based on the rock toughness. The proposed empirical model was validated by comparing the predicted and measured UCS values of experimentally tested rocks, and the comparison showed a good agreement with a mean bias (the ratio of measured to the predicted compressive strength) of 1.002.
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