在二维摩擦模型中的近周期性紧缩事件
Sean McNamara1, Renaud Delannay1
1Université de Rennes, CNRS, IPR [(Institut de Physique de Rennes)]-UMR 6251, F-35000 Rennes, France.
Physical review. E
|September 16, 2025
概括
研究人员开发了一种2D模型来模拟雪崩前体,雪崩前体是颗粒状材料中的表面位移. 该模型成功地重现了这些事件,并揭示了摩擦,系统大小和前体行为之间的关系.
科学领域:
- 颗粒状材料的物理学 颗粒状材料的物理学
- 复杂系统的动态 复杂系统的动态
- 计算物理学的计算物理.
背景情况:
- 雪崩的前体,其特点是半周期性地表移位,在颗粒床的缓慢倾斜过程中观察到.
- 尽管自2000年代中期以来一直在进行实验研究,但这些前体的数值模型仍然具有挑战性.
- 以前的尝试包括简化的一维模型,这些模型不能完全捕捉实验设置的复杂性.
研究的目的:
- 开发一个更现实的二维数值模型来模拟雪崩前体.
- 调查在颗粒系统中管理前体事件的潜在机制和定量关系.
- 为了弥合简化1D模型和复杂的3D实验观测之间的差距.
主要方法:
- 创建了一个二维离散元素模型,模拟了与颗粒分子动力学相互作用的摩擦平面上的磁盘.
- 该模型结合了邻近磁盘和边界之间的相互作用.
- 在颗粒床的缓慢倾斜下进行模拟,以观察前体事件.
主要成果:
- 该模型强大地复制了准周期性紧缩事件,被确定为雪崩前体.
- 事件之间的角周期与静态和动态摩擦系数之间的差异成正比.
- 系统大小影响前体的行为,较大的系统在初始事件时呈现下降的倾斜度和减少的角周期.
结论:
- 开发的2D模型为了解雪崩前体现象提供了有价值的工具.
- 摩擦系数和系统大小等关键参数显著影响前体事件的特征.
- 该模型能够复制实验观测,包括循环倾斜效应的能力,验证了其方法.
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