在存在固体-流体边界的情况下,地震波场的高效混合数值建模
Chao Lyu1, Barbara Romanowicz2,3, Liang Zhao4
1Department of Earth and Planetary Science, University of California, Berkeley, CA, USA. lyuchao1988@gmail.com.
Nature communications
|February 18, 2025
概括
盒子断层学,一种混合的地震成像方法,通过将波场计算分解成部分,显著降低了计算成本. 这项研究统一了混合模拟的固体-流体合,使复杂的地球区域的精确地质物理成像成为可能.
科学领域:
- 地质物理学 地质物理学
- 计算地震学计算地震学
- 地球科学 地球科学 地球科学
背景情况:
- 全波形地震成像需要在很远的距离上对波场进行广泛的计算.
- 目前用于3D模型中的地震波场计算的数值方法是计算密集的.
- 绘制小规模地质物理结构的图像需要高效的波场计算方法.
研究的目的:
- 为混合地震模拟开发一个统一的框架,包括固体-流体合.
- 为具有流体-固体边界的区域适应"盒子断层"方法.
- 为了降低地震波场计算的计算成本,而不会牺牲准确性.
主要方法:
- 对声波方程解决方案的位移电位表达式的调和.
- 为混合数值模拟开发一个统一的框架.
- 对海底和核心-地幔边界的目标区域进行基准测试混合模拟.
主要成果:
- 建立了一个统一的框架,用于混合模拟跨流体-固体边界的地震波传播.
- "盒子断层扫描"方法已成功适用于复杂的地质区域.
- 与标准方法相比,计算成本减少了一千倍,并保持准确性.
结论:
- 统一的框架显著提升了"盒子断层学"在任意地球区域的适用性.
- 这种方法使得小规模结构的地震成像能够准确且计算效率高.
- 该方法通过在关键的地球物理界面 (如海洋底和核心-地幔界限) 的基准来验证.
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