介面级雪崩的大小支了颗粒性产量的重力学
1Department of Mechanical Engineering, National Chung Hsing University, Taichung 402202, Taiwan.
概括
颗粒状材料在屈服之前显示了不同大小的雪崩. 一个新的模型统一了雪崩动力学和散装风学,揭示了中层雪崩演变是颗粒性产量的关键.
科学领域:
- 物理 物理学 物理
- 材料科学 材料科学 材料科学
- 地质物理学 地质物理学
背景情况:
- 颗粒状材料在屈服之前会出现间歇性的雪崩,类似于像山体滑坡这样的自然故障.
- 现有的模型有效地描述了产量后的流量,但缺乏统一的框架来描述产量前的动态和散装质学.
研究的目的:
- 开发一个统一的构成模型,将产量前的雪崩动态与颗粒材料中的散装形学联系起来.
- 研究从间歇性雪崩过渡到连续的塑料流.
主要方法:
- 一个双断裂的双剪切实验被用来探测雪崩统计数据和在收益过渡附近的准静态流.
- 分析的重点是雪崩的大小分布和不同剪速下的流动行为.
主要成果:
- 雪崩模式表现出速度减弱的行为,而塑料模式是独立于速度的,表明双重的风湿学.
- 在相同的局部剪切速率下观察到歇斯底里和机械不稳定性.
- 平均正常化应力下降被确定为一个关键变量,弥合了雪崩和塑料制度.
结论:
- 制定了一个统一的构成模型,成功地捕捉了颗粒材料中的整个产量过渡.
- 中级雪崩的演变被确立为控制颗粒性产量流动学的中心机制.
- 结果提供了对自然故障现象和物质不稳定性的洞察.
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