Compression Mechanical Properties and Constitutive Model for Soft–Hard Interlayered Rock Mass

IF 16.4 1区 化学 Q1 CHEMISTRY, MULTIDISCIPLINARY
Jinhua Li, Yang Yang, Pan Wang, Tianyu Zhang, Peili Su, Songwei Zhao
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Abstract

The properties of soft–hard interbedded rock masses are significantly impacted by the strength of rock layers and the characteristics of interface surfaces. This study investigates the mechanical properties of soft–hard interlayered rock masses by preparing rock-like specimens with different interface angles. Uniaxial and triaxial compression tests were conducted to examine the compression mechanical characteristics of the specimens. Experimental results demonstrated that in the uniaxial compression tests, the peak strength of the two-layer rock-like specimen exhibits an initial decrease followed by an increase as the interface angle increases. Similarly, the peak strength of the three-layer rock-like specimen also follows a “U-shaped” pattern. The failure of both specimens shifts from tensile failure to shear failure. In the triaxial tests, the strength of the two-layer rock-like specimen initially increases and subsequently decreases as the interface angle increases. In contrast, the intensity of the three-layer rock-like specimen exhibits a decreasing trend, transitioning from shear dilation or tensile failure to shear failure. By utilizing the damage constitutive model to compute the compressive strength of the composite specimen, it was observed that the deviation from the experimental value did not exceed 2.5%, and the overall shape of the curves was in good agreement. Consequently, it is affirmed that the damage constitutive model developed in this study can accurately capture the pre-peak phase of the stress–strain relationship in soft–hard interlayered rock-like specimens, thus providing a valid representation of their mechanical behavior.
软硬夹层岩体的压缩力学性能和构造模型
软硬夹层岩体的特性受到岩层强度和界面表面特征的显著影响。本研究通过制备不同界面角度的类岩试样,研究软硬夹层岩体的力学特性。通过单轴和三轴压缩试验来检验试样的压缩力学特性。实验结果表明,在单轴压缩试验中,随着界面角的增大,两层类岩石试样的峰值强度先降低后升高。同样,三层类岩石试样的峰值强度也呈 "U "型。两种试样的破坏都从拉伸破坏转变为剪切破坏。在三轴试验中,两层类岩石试样的强度最初随着界面角的增大而增大,随后随着界面角的增大而减小。相比之下,三层类岩石试样的强度呈下降趋势,从剪切扩张或拉伸破坏过渡到剪切破坏。通过利用损伤构成模型计算复合试样的抗压强度,发现与实验值的偏差不超过 2.5%,曲线的整体形状也非常吻合。因此,本研究建立的损伤构成模型可以准确捕捉软硬夹层岩类试样应力-应变关系的前峰值阶段,从而有效地反映其力学行为。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Accounts of Chemical Research
Accounts of Chemical Research 化学-化学综合
CiteScore
31.40
自引率
1.10%
发文量
312
审稿时长
2 months
期刊介绍: Accounts of Chemical Research presents short, concise and critical articles offering easy-to-read overviews of basic research and applications in all areas of chemistry and biochemistry. These short reviews focus on research from the author’s own laboratory and are designed to teach the reader about a research project. In addition, Accounts of Chemical Research publishes commentaries that give an informed opinion on a current research problem. Special Issues online are devoted to a single topic of unusual activity and significance. Accounts of Chemical Research replaces the traditional article abstract with an article "Conspectus." These entries synopsize the research affording the reader a closer look at the content and significance of an article. Through this provision of a more detailed description of the article contents, the Conspectus enhances the article's discoverability by search engines and the exposure for the research.
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