在地质过程中出现前体不稳定性的出现:来自密集活性物质的洞察
Klaus Regenauer-Lieb1, Manman Hu2
1WA School of Mines: Minerals, Energy and Chemical Engineering, Energy Engineering Discipline, Curtin University, Perth, 6151, WA, Australia.
Heliyon
|December 13, 2023
概括
现在可以研究地质过程中大规模不稳定的前体机制. 这些在密集活性物质中观察到的前体,表现为源自特殊点的自我激发波.
科学领域:
- 地质物理学 地质物理学
- 固体力学 固体力学是什么
- 非平衡的热力学 热力学
背景情况:
- 地理过程中的大规模不稳定性往往缺乏理解的前体机制.
- 密集的活性物质,远离平衡,表现出复杂的行为.
- 固体力学中的波动不稳定性与特有值凝聚在一起的特殊点有关.
研究的目的:
- 调查大规模地质过程不稳定的被忽视的前体机制.
- 探索密集活性物质中自我激发波的现象.
- 为了将微观前体过程与宏观不稳定性联系起来.
主要方法:
- 在外部强迫下对密集活性物质进行建模.
- 在多孔介质中合固体和流体压力的标量场变量.
- 将Onsager定理扩展到非本地过程中.
主要成果:
- 在多元组件材料中确定了远离平衡的前体过程.
- 观察到自我激发波和与宏观梯度的动态不相容.
- 发现了振荡式指数增长的波动,在特殊点形成核.
结论:
- 为非局部过程提出了一个严格的理论,扩展了Onsager的定理.
- 异常点对于复杂的并联固有模式的开始至关重要.
- 未来的工作包括实验验证和用于检测前体的传感器开发.
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