强烈地震后岩石中的声学参数放松
Andrey V Lebedev1, Lev A Ostrovsky2,3
1Gaponov-Grekhov Institute of Applied Physics, Russian Academy of Sciences, Nizhny Novgorod, Russia.
The Journal of the Acoustical Society of America
|March 19, 2025
概括
地震波的速度在地震后发生变化,并在几个月到几年内慢慢恢复. 一个基于谷物接触演变的物理模型准确地模拟了这种恢复,帮助岩石应力诊断.
科学领域:
- 地质物理学 地质物理学
- 岩石机械学 岩石机械学
- 地震学 地震学
背景情况:
- 地震波的速度在地震后发生变化.
- 恢复地震波速度是一个缓慢的过程 (几个月到几年).
- 在实验和自然中观察到的地震波速度恢复的对数时间依赖性.
研究的目的:
- 分析地震波速度恢复的实验和观测数据.
- 应用基于Arrhenius类型方程的物理模型来描述这种现象.
- 验证模型模拟岩石中放松过程的能力.
主要方法:
- 对地震波速度变化的实验结果的分析.
- 利用来自帕克菲尔德地震天文台的长期观测数据.
- 采用基于Arrhenius类型方程的物理模型,用于接触进化.
主要成果:
- 对地震波速度恢复时间的模拟显示了与实验数据的满意一致.
- 物理模型成功地描述了实验室实验中观察到的缓慢时间效应.
- 该模型的预测与长期的地震观测结果一致.
结论:
- 开发的物理模型准确地捕捉了地震波速度恢复动态.
- 该模型为了解地震后放松过程提供了一个框架.
- 研究结果表明,使用地震数据,有可能对岩石应力状态进行远程诊断.
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