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Strain localization in soft rock-a typical rate-dependent solid: experimental and numerical studies

机译:软岩中的应变局部化-一种典型的速率相关固体:实验和数值研究

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摘要

Strain localization developing inside soft rock specimens is examined through experimental observation and numerical simulation. In the experimental study, soft rock specimens are sheared at different strain rates under plane strain conditions and deformation and strain localization characteristics are analysed. Transition of localization mode from highly localized mode for higher strain rate to distributed and diffused mode of strain localization for lower strain rates was observed. In the numerical study, simulations of plane strain compression tests are carried out at different strain rates by using an overstressed-type elasto-viscoplastic model in finite element computations. The role of strain rates on setting gradients of strain fields across shear band is clarified. The probable mechanism for transition of localization mode is discussed.
机译:通过实验观察和数值模拟检查了软岩标本内部发生的应变局部化。在实验研究中,软岩标本在平面应变条件下以不同的应变速率剪切,并分析了变形和应变局部化特征。观察到定位模式从较高应变率的高度局部化模式过渡到较低应变率的应变局部化的分散模式。在数值研究中,通过在有限元计算中使用超应力型弹黏塑性模型,在不同应变率下进行了平面应变压缩试验的模拟。阐明了应变速率在设定整个剪切带上应变场梯度上的作用。讨论了定位模式转换的可能机制。

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