晶体可塑性的近周期性事件和自组织的雪崩振荡器
Stefanos Papanikolaou1, Dennis M Dimiduk, Woosong Choi
1Department of Mechanical Engineering and Materials Science, Yale University, New Haven, Connecticut 06520-8286, USA. stefanos.papanikolaou@yale.edu
Nature
|October 27, 2012
概括
压力系统中的雪崩可能会受到缓慢放松过程的影响. 这项研究揭示了一个新的"自我组织的雪崩振荡器"临界状态,影响物质和地质事件中的雪崩动态.
科学领域:
- 材料科学 材料科学 材料科学
- 凝聚物质物理学 凝聚物质物理学
- 地质物理学 地质物理学
背景情况:
- 系统中的外部压力通常通过被称为雪崩的突然,冲动事件来缓解.
- 然而,这些事件之间可能会发生缓慢的放松过程,从而影响雪崩的行为.
- 例如,地震之间的水流和水晶中的脱位流.
研究的目的:
- 实验性地研究缓慢放松对应力系统中雪崩动态的影响.
- 探索新的关键状态及其属性的出现.
- 开发和验证一个包含缓慢放松的理论模型.
主要方法:
- 微晶的实验压缩在延展率的三个数量级.
- 脱位雪崩的分析和计算建模,扩展到包括脱位放松.
- 准周期性雪崩爆发和临界指数的观测和分析.
主要成果:
- 在微晶体中观察到非常规的半周期性雪崩爆发.
- 随着应变率的下降,注意到更高的临界指数,表明临界行为发生了变化.
- 经过验证的实验结果与精细的脱位雪崩模型.
结论:
- 发现了一个新的关键状态:自组织的雪崩振荡器.
- 这种状态表现出向一个决定关键点的振荡式方法.
- 这些发现表明,当雪崩与缓慢放松竞争时,准周期性规模不变性出现,适用于微塑性和地震等多种系统.
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