概括
在1987年的迷信山地震中,过度的孔水压力是土壤液化的一个关键因素,在强烈的地震震动结束后,积累到石静态水平. 这种液化发生在水平加速超过关键值时.
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:
- 土壤液化是一种在地震期间和土壤失去强度和刚性的现象.
- 了解孔水压力动态对于预测液化及其对基础设施的影响至关重要.
- 迷信山地震提供了一个独特的机会,可以实时研究液化过程.
研究的目的:
- 为了研究地震加速和液化过程中的孔水压力变化之间的关系.
- 为了确定水平加速的门,触发过多的孔水压力产生.
- 分析相对于强烈地震运动而形成孔水压力的时间.
主要方法:
- 同时测量孔水压力和表面/地下加速.
- 现场监测证实某个地点正在进行液化.
- 在1987年迷信山地震 (M = 6.6) 期间记录的数据分析.
主要成果:
- 孔隙总压力达到石静态条件,表明土壤强度几乎完全丧失.
- 意想不到的是,峰值孔隙压力发生在最强烈的地震运动停止后.
- 过度的孔隙压力仅在水平加速超过特定值后才产生.
结论:
- 地震液化与超过关键水平加速值密切相关.
- 孔隙压力积累的时间表明,在初始震动后,反应延迟或积累效应.
- 这些发现对地震设计规范和危险评估有重大影响.
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