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Shock Wave Application to Cell Cultures
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用线性波传播模型复制明显的非线性地震反应
1U.S. Bureau of Reclamation, Box 25007 D-8330, Denver, CO 80225, USA.
概括
沉积物中的地面运动放大可能看起来非线性,但通过随机的3D地变化通过线性波传播来解释. 这一发现对于地震工程中精确的地震负载预测至关重要.
科学领域:
- 地震学 地震学
- 地震工程的工程是地震工程.
- 地质物理学 地质物理学
背景情况:
- 了解沉积物的地面运动放大对于预测地震负载至关重要.
- 在诺斯里奇地震期间观察到的放大显示了明显的非线性行为,较弱的余震比主震造成更大的影响.
研究的目的:
- 研究沉积物观察到的地面运动放大背后的机制.
- 确定线性波传播是否可以解释明显的非线性沉积物反应.
主要方法:
- 使用实证冲动反应进行地震模拟.
- 弹性有限差异计算包括随机的三维 (3D) 地速度变化.
主要成果:
- 通过随机3D速度变化的线性波传播成功地解释了观测到的地面运动放大.
- 这个模型还复制了峰值地面运动的日志正常分散.
结论:
- 显而易见的非线性沉积物反应可以归因于异质介质中的线性波传播.
- 确定性模型不足以量化近源地面运动的扩展和分散.
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