地震波在超深处的传播特征被大规模的摇摆桌试验
Yang Xing1, Li Wentao2, Wu Shibin3
1Power China Chengdu Engineering Corporation Limited, Chengdu, 610072, People's Republic of China.
Scientific reports
|July 2, 2025
概括
在深度超载中地震波的传播因方向而异. 水平波被过,而垂直波在顶部显示出更高的峰值加速,高频过较弱,影响土岩大的地震性能.
科学领域:
- 地质技术工程 地质技术工程
- 地震学 地震学
- 地震工程的工程是地震工程.
背景情况:
- 在深度超负荷上的土岩需要了解地震波传播,以便进行动态响应分析.
- 在深度超负荷下地震波的行为对于大的安全性和性能评估至关重要.
研究的目的:
- 在深度超负荷下研究地震波传播特征 (水平和垂直).
- 分析深层超负荷对地震波调制和孔隙压力响应的影响.
主要方法:
- 进行了大规模的摇摆桌测试.
- 分析涉及使用斯托克威尔变换和连贯函数方法的加速和孔隙压力数据.
主要成果:
- 水平的地震波显示了振幅调制和强大的高频过,低频率主导.
- 垂直地震波在顶部呈现出更高的峰值加速,高频波较弱.
- 过多的孔隙压力积累在深度上是相似的,但液化只发生在超负荷顶部.
结论:
- 深度超负荷在水平和垂直方向上显著调节地震波.
- 弱层间层有效地过高频水平地震波.
- 了解这些异构波传播效应对于深度超负荷大的地震设计至关重要.
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