从秒到几十年九层混凝土建筑的自然频率变化

E. Williams, T. Heaton, Z. Zhan, Valère Lambert
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引用次数: 2

摘要

自2001年以来,南加州地震台网已经存档了强震台站CI的连续波形数据。MIK位于加州理工学院大厅(原密立根图书馆),一栋九层钢筋混凝土建筑。对这20年记录的简单频谱分析显示,建筑物的基本频率逐渐增加了5.1%(东西方向)和2.3%(南北方向),长期变化较大,达到9.7%(东西方向)和4.4%(南北方向)。这一发现是出乎意料的,因为之前对强迫振动测试和强震记录的分析表明,在1968年至2003年之间,基频下降了22%(东西方向)和12%(南北方向),这主要归因于轻微的结构破坏和大地震引起的土壤结构系统变化。如今,这座建筑的表面结构刚度与1986年惠蒂尔海峡地震发生前的水平相当。利用地震和强迫振动的数据,我们还记录了建筑物的非线性动态弹性,其特点是在强烈运动开始时迅速软化(表观频率降低),随后在几分钟内缓慢的对数线性恢复趋势。这种非线性行为似乎并没有随着时间而改变。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Variability in the Natural Frequencies of a Nine-Story Concrete Building from Seconds to Decades
Since 2001, the Southern California Seismic Network has archived continuous waveform data from strong-motion station CI.MIK in Caltech Hall (formerly Millikan Library)—a nine-story reinforced concrete building. Simple spectral analysis of this 20 yr record reveals that the building’s fundamental frequencies have increased gradually by 5.1% (east–west) and 2.3% (north–south), with larger long-term variability up to 9.7% (east–west) and 4.4% (north–south). This finding is unexpected, as previous analysis of forced vibration tests and strong-motion records has shown that between 1968 and 2003 the fundamental frequencies decreased by 22% (east–west) and 12% (north–south), largely attributed to minor structural damage and soil–structure system changes from major earthquakes. Today, the building’s apparent structural stiffness is comparable to what it was in 1986, before the Whittier Narrows earthquake. Using data from earthquakes and forced vibrations, we also document the building’s nonlinear dynamic elasticity, which is characterized by a rapid softening (decrease in apparent frequencies) at the onset of strong motion, followed by a slower, log–linear recovery trend over the scale of minutes. This nonlinear behavior does not appear to have changed with time.
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