在膨胀/收缩周期下,颗粒状物质的下坡爬行
1Centro Atómico Bariloche, Instituto Balseiro, Comisión Nacional de Energía Atómica, CNEA, CONICET, UNCUYO, Av. E. Bustillo 9500 (R8402AGP) San Carlos de Bariloche, Río Negro, Argentina. jagla@cab.cnea.gov.ar.
Soft matter
|November 27, 2023
概括
颗粒状物质在粒子大小波动时爬下坡. 这种由尺寸变化驱动的同步运动在表面最强,并且随着深度的增加而减少.
科学领域:
- 物理 物理学 物理
- 地质物理学 地质物理学
- 材料科学 材料科学 材料科学
背景情况:
- 在重力下的颗粒状材料可以表现出复杂的行为.
- 表面条件可以影响颗粒状土壤的动态.
- 了解爬行机制对于地质工程至关重要.
研究的目的:
- 为了研究倾斜的颗粒层的下坡爬行.
- 探索准静态振荡粒子大小变化对爬行的影响.
- 分析这种爬行现象的深度依赖性.
主要方法:
- 模拟颗粒物质作为软盘的二维多分散系统.
- 模拟粒子的半静态振荡大小变化,在表面最大,在深度下降.
- 测量每周期的爬行前进作为斜率角度和粒子大小变化的函数.
主要成果:
- 颗粒系统表现出同步的下坡爬行,以响应振荡粒子大小变化.
- 爬行速度取决于斜率角度和粒子大小变化的程度.
- 爬行速度在表面是最高的,并且随着深度的增加而减少.
结论:
- 准静态振荡粒子大小变化可以诱导颗粒材料的下坡爬行.
- 观察到的依赖深度的爬行行为模仿了在颗粒状土壤中的现场观测.
- 这项研究提供了对驱动颗粒物质运输的新机制的见解.
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