首页|基于HHT的典型红土区地脉动特性与场地特征关联性研究

基于HHT的典型红土区地脉动特性与场地特征关联性研究

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对典型红土场地开展系统的地脉动测试,基于希尔伯特-黄变换(Hilbert-Huang transform,HHT)中的经验模态分解(empirical mode decomposition,EMD)从测试信号中分解出场地有效地脉动信号,对其进行快速傅里叶变换(fast Fourier transform,FFT)和Hilbert变换,产生功率谱曲线和Hilbert边际谱曲线,以确定场地卓越周期,进而探索与直接傅氏法和H/V谱比法不同的场地特征参数判别方法.目标场地的有效地脉动信号为 EMD 分解后的第 4 个本征模态函数(4th intrinsic mode function,IMF4),对各个测点的IMF4 进行FFT和Hilbert变换,获取的地脉动卓越周期水平向在 0.20~0.36 s,垂直向在 0.23~0.39 s,结果表明,基于HHT的地脉动测试法来确定场地类别、划分场地岩土类型,与场地钻孔分析结果一致性高,关联性强.
Study on correlation between microtremor characteristics and site characteristics in typical laterite areas based on HHT
A systematic microtremor measurement was conducted on typical laterite sites.The empirical mode decomposition(EMD)in Hilbert Huang transform(HHT)was used to decompose the effective microtremor signals from the measurement signals.Fast Fourier transform(FFT)and Hilbert transform were used to ge-nerate power spectral curves and Hilbert marginal spectral curves of the effective microtremor signal to deter-mine the predominant period of the site,and then to explore methods for determining site characteristic param-eters that are different from the direct Fourier methods and H/V spectral ratio methods.The effective micro-tremor signal of the target site is the fourth intrinsic mode function(IMF4)derived from EMD.The predomi-nant period of microtremor obtained by FFT and Hilbert transformation on the IMF4 of each measurement point ranges from 0.20~0.36s in the horizontal direction and from 0.23~0.39s in the vertical direction.Such results indicate that the determination of site classification and division of geotechnical types through microtremor measurement based on HHT is highly consistent and correlated with the drilling results of the site.

microtremorsite characteristicsHHTpredominant periodlaterite areas

周仰新、李永强、许言、刘旭锋、陈波

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东华理工大学 土木与建筑工程学院,江西 南昌 330013

南昌市应急管理局,江西 南昌 330038

地脉动 场地特征 HHT 卓越周期 红土区

国家自然科学基金江西省"双千计划"项目江西省自然科学基金

52068002DHSQT32022006/JXSQ202010104120202BABL204064

2024

福建工程学院学报
福建工程学院

福建工程学院学报

影响因子:0.318
ISSN:1672-4348
年,卷(期):2024.22(1)
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