在二维波导中对联模式分离多重分散波场组件
1Stockholm University, Stockholm 11529, Sweden.
Royal Society open science
|October 6, 2023
概括
本研究介绍了一种数学精确的方法,用于分析水平不变波导中的波散射. 该技术精确地模拟了地震波放大局部异常的模型,如没有高频近似的流谷.
科学领域:
- 地质物理学 地质物理学
- 波浪传播 波浪传播
- 计算地震学计算地震学
背景情况:
- 在异质介质中的波传播对于理解地震波现象至关重要.
- 当地的地质异常,如流山谷,可以显著放大地震地面运动.
- 对多重散射的准确建模对于地震危险评估至关重要.
研究的目的:
- 开发一个数学精确的部分波分解,用于分析波导中的波场行为.
- 评估由水平移动的介质异常引起的多重散射效应.
- 提供适用于地震波传播和地面运动研究的方法.
主要方法:
- 波场的部分波分解.
- 离散合模式理论和反射/传输矩阵.
- 避免高频射线近似,确保数学准确性.
- 全球优化用于人工媒介终止的应用.
- 对发生平面波的水平源数组的导出.
主要成果:
- 在水平不变波导中分析波散射的新,数学精确的方法.
- 该方法准确地模拟了多重散射,而不依赖于高频近似.
- 通过诸如流山谷等地质异常来扩大地震波的适用性.
- 扩展涉及贝塞尔函数的里埃变换关系.
结论:
- 提出的部分波分解为研究复杂介质中的波传播和散射提供了强大而准确的工具.
- 该方法为分析二维异常形状的纯数值技术提供了有价值的替代方案.
- 这些发现对理解和预测地震地面运动放大有直接影响.
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