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高精度检测地球的自由振荡信号,考虑相位一致性
Yaxin Zhao1, Gong Xu1, Hanwei Zhang1
1School of Civil Engineering and Spatial Information, Shandong University of Technology, Zibo 255000, China.
Sensors (Basel, Switzerland)
|January 28, 2026
概括
本研究引入了一种结合正常时间频率转换 (NTFT) 和最佳序列估计 (OSE) 的新方法,用于精确检测地球.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地球的深层内部地球的深层内部.
背景情况:
- 对地球正常模式的高精度检测对于理解深层内部结构至关重要.
- 像最佳序列估计 (OSE) 这样的现有方法可能会受到异步振荡的影响.
- 超导重力仪数据为地震分析提供高分辨率测量.
研究的目的:
- 开发一种高精度的方法来检测地球的正常模式.
- 为了解决异步振荡对正常模式检测精度的影响.
- 通过增强的地震数据分析,提高对地球深层内部结构的理解.
主要方法:
- 组合正常时间频率转换 (NTFT) 和最佳序列估计 (OSE).
- 使用NTFT从超导重力仪数据中提取瞬间相位光谱.
- 阶段一致性被整合到OSE方法中,以考虑检测到的异步振荡.
主要成果:
- 使用NTFT确认了正常模式中的异步振荡,影响了OSE的准确性.
- 综合NTFT-OSE方法成功考虑了相位一致性.
- 对3S1模型 (m = -1,0,1) 的单片频率在0.9424mHz,0.944mHz和0.9455mHz准确地检测到,显示出与PREM理论值的良好一致.
结论:
- 拟议的NTFT-OSE方法通过解决相位一致性,提供高精度的正常模式检测.
- 这种技术验证了考虑相位一致性的有效性,以进行准确的地震分析.
- 这些发现为探索地球深层结构和改进地球模型提供了关键数据和技术支持.
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