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首页> 外文期刊>Geophysical Research Letters >Incremental propagation of discrete compaction bands: Acoustic emission and microstructural observations on circumferentially notched samples of Bentheim - art. no. 1775
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Incremental propagation of discrete compaction bands: Acoustic emission and microstructural observations on circumferentially notched samples of Bentheim - art. no. 1775

机译:离散压实带的增量传播:本特海姆艺术的周向缺口样品的声发射和显微结构观察。没有。 1775年

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1] To simulate how compaction localization may develop from structural and stress heterogeneity, we studied in the laboratory the influence of a stress concentration due to a V-shaped circumferential notch in a cylindrical sample of Bentheim sandstone. Conventional triaxial experiments at confining pressure of 300 MPa were conducted. Acoustic emission activity was recorded, and each sample was deformed to a different stage and subsequently retrieved for microstructural observations. Our data indicate that compaction bands initiated from the notch tips and propagated by sequential increments as "anti-cracks''. The transverse propagation of a compaction band was inferred to be faster than the axial displacement rate by 2 orders of magnitude. Energy dissipated for compaction band formation was estimated to be comparable to the shear fracture energy for shear band propagation. [References: 22
机译:1]为了模拟结构和应力异质性如何引起压实局部化,我们在实验室研究了Bentheim砂岩圆柱状样品中V形周向缺口对应力集中的影响。在围压为300 MPa的条件下进行了常规三轴实验。记录声发射活性,并将每个样品变形到不同的阶段,然后取回进行显微结构观察。我们的数据表明,压实带从缺口尖端开始,并以“抗裂”的形式依次传播,据推测,压实带的横向传播比轴向位移速率快两个数量级。估计压实带的形成与剪切带传播中的剪切断裂能相当[参考文献:22

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