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首页> 外文期刊>Bulletin of engineering geology and the environment >Mechanical behavior of Benxi Formation limestone under triaxial compression: a new post-peak constitutive model and experimental validation
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Mechanical behavior of Benxi Formation limestone under triaxial compression: a new post-peak constitutive model and experimental validation

机译:本溪组石灰岩三轴压缩作用下的力学行为:一个新的峰后本构模型和实验验证

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摘要

In order to understand the mechanical behavior of limestone and to formulate a new post-peak constitutive model, triaxial tests on the intact Benxi Formation limestone from Gequan mine, Hebei Province, China, were conducted using the Electro-hydraulic Servo-controlled Rock Mechanics Testing System (MTS815). Test results showed that the deformation behavior of the limestone specimens at the post-peak stage was that the axial stress dropped rapidly and the axial strain remained constant for some time before it continued to grow, but lateral strain kept increasing. To explain the deformation behavior and failure mechanism of the intact specimens, mineral composition and microstructure were analyzed using both a polarizing optical microscope and scanning electron microscopy. A tension-shear failure strength criterion was established based on the observed failure modes of the intact specimens. Furthermore, a new post-peak constitutive model was proposed according to the deformation behavior of the intact specimens at the post-peak stage. The proposed post-peak constitutive model was further developed by considering both failure strength criterion and confining pressure. In order to validate the proposed model, experimental data and theoretical results predicted by the proposed model were compared. Comparison of results showed that the new model can capture the post-peak deformation behavior of the limestone well. Additionally, repeated loading tests under triaxial compression were performed to investigate the influence of loading times on the mechanical behavior of the fractured limestone specimens. Test results showed that both the maximum load and plastic deformation of the fractured specimens decreased with increasing loading times.
机译:为了理解石灰石的力学行为并建立新的峰后本构模型,使用电液伺服控制岩石力学试验对河北葛泉矿完整的本溪组石灰岩进行了三轴试验。系统(MTS815)。试验结果表明,石灰岩试件在峰后阶段的变形行为是:轴向应力迅速下降,轴向应变在持续增长之前保持一定的时间,但横向应变却持续增加。为了解释完整样品的变形行为和破坏机理,使用偏光光学显微镜和扫描电子显微镜分析了矿物成分和微观结构。基于观察到的完整试样的破坏模式,建立了拉伸剪切破坏强度准则。此外,根据峰后阶段完整样本的变形行为,提出了一个新的峰后本构模型。通过同时考虑破坏强度准则和围压,进一步发展了所提出的峰后本构模型。为了验证所提出的模型,比较了所提出的模型的实验数据和理论结果。结果比较表明,新模型可以很好地捕获石灰岩的峰后变形行为。另外,在三轴压缩下进行了重复的载荷试验,以研究载荷时间对破裂的石灰岩试样力学性能的影响。试验结果表明,随着载荷时间的增加,断裂试样的最大载荷和塑性变形均减小。

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