摩擦滑动是如何演变的
Songlin Shi1, Meng Wang1, Yonatan Poles1
1The Racah Institute of Physics, The Hebrew University of Jerusalem, Givat Ram, Jerusalem, 91904, Israel.
Nature communications
|December 13, 2023
概括
地震断裂是由许多小的,次要的断裂驱动的,而不仅仅是最初的滑动. 了解这些次要事件是解释总滑动和余震在断层运动中的作用的关键.
科学领域:
- 地质物理学 地质物理学
- 部落学 (tribology) 是一个学科.
- 断裂力学 断裂力学 断裂力学
背景情况:
- 摩擦接口控制着滑运动,这对于理解地震至关重要.
- 棒滑事件中的初始滑动往往小于事件的总滑动,随后的运动归因于动态摩擦.
- 持续滑动的基本机制和二次破裂的作用仍然不完全理解.
研究的目的:
- 为了研究二次破裂在摩擦滑动中的作用.
- 在stick-slip事件中直接测量真实接触面积和界面上的滑动.
- 阐明二次破裂,接触面积和应变变异之间的关系.
主要方法:
- 在摩擦界面直接测量实际接触面积.
- 在摩擦界面直接测量滑动.
- 应用断裂力学原理来分析滑动增量和接触面积变化.
主要成果:
- 在最初的破裂之后,大量的,以前未被检测到的二次破裂的序列立即触发.
- 每次二次断裂都会产生渐进的滑动,从而导致整体接口运动.
- 滑动的增加与接触区域和局部应变的变化直接相关,由断裂力学解释.
结论:
- 在stick-slip事件中积累的接口滑动只能通过计算二次断裂来准确地描述.
- 这些发现提供了关于摩擦运动的基本见解,以及余震在地震滑动发生中的重要性.
- 该研究重新定义了对自然断层系统中滑动动态的理解.
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