在三维减弱弹性介质中,压缩和剪切波之间的能量分割
Roel Snieder1, Marine Deheuvels2
1Center for Wave Phenomena, Colorado School of Mines, Golden, Colorado 80401, USA.
The Journal of the Acoustical Society of America
|May 17, 2024
概括
衰减显著影响弹性介质中的地震波能量比率. 这项研究表明,切削波 (S波) 与压缩波 (P波) 的能量比率在存在衰减时偏离理论值,特别是在动态和平衡状态下.
科学领域:
- 地震学 地震学
- 波传播物理学 波传播物理学
- 声学 声学 声学 声学
背景情况:
- 在非减弱弹性介质中,地震波场以剪切波 (S波) 为主.
- 在3D中,S波与压缩波 (P波) 的能量比率在没有衰减的情况下从理论上定义为ES/EP=2(vP/vS) 3.
研究的目的:
- 为了研究衰减对S波与P波能量比率的影响.
- 分析衰减如何影响这种比率,无论是在短暂 (回归) 和稳定状态 (能量平衡) 条件下.
主要方法:
- 在衰减的存在下,波浪能量演变的数学建模.
- 分析指导的里卡蒂方程,用于能量比,在回归模式下.
- 研究能量平衡的条件,考虑衰减和能量注入速度.
主要成果:
- 在回归模式下,能量比遵循里卡蒂方程,而不是指数衰减.
- 如果P波和S波的衰减系数不同,长时间能量比率会偏离非衰减值.
- 当波浪平衡速度快或当能量注入平衡每个波浪类型的消散时,就会实现能量平衡.
结论:
- 衰减从根本上改变了地震波能量分区,偏离了理想弹性介质的预测.
- 对于P波和S波的不同衰减率的存在对于理解长期能量比率至关重要.
- 了解这些效应对于在现实的地球材料中准确地解释地震波场至关重要.
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