摩擦的直接效应是否随着绝对温度的不断增加而不断增加?
1Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740.
概括
断层摩擦的直接影响在很大程度上独立于温度,与经典模型相反. 不同的变形机制,而不是温度,在岩石破裂时驱动摩擦变化.
科学领域:
- 地质物理学 地质物理学
- 岩石机械 岩石机械
- 地震学 地震学
背景情况:
- 断层摩擦的构成模型对于基于物理的地震模拟至关重要.
- 广泛采用的框架假定一个热激活的过程由阿雷尼乌斯定律,预测温度依赖的摩擦.
- 这种古典观点表明,摩擦的直接影响随着绝对温度的增加而增加.
研究的目的:
- 实验测试故障摩擦中直接效应的温度依赖性.
- 研究岩石中摩擦,温度和变形机制之间的关系.
- 挑战经典的基于阿雷尼乌斯定律的断层摩擦模型.
主要方法:
- 在各种水热,气流和岩石学条件下分析综合实验室数据.
- 在不同温度和压力下检查故障摩擦行为.
- 识别与脆性和半脆性过渡相关的明显变形机制.
主要成果:
- 对于给定的变形机制,摩擦的直接作用在很大程度上与温度无关.
- 直接效应的增量转移与脆性到半脆性的过渡相关.
- 截然不同的变形机制在这个过渡过程中运行,影响摩擦行为.
结论:
- 热激活摩擦的经典模型 (Arrhenius定律) 受到实验证据的挑战.
- 断层摩擦主要由运行变形机制而不是绝对温度来控制.
- 石质层岩石破裂的现实构成规律必须整合在断层区域中活跃的多种变形机制.
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