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Empirical estimation of the Newmark displacement from the Arias intensity and critical acceleration

机译:根据Arias强度和临界加速度对Newmark位移的经验估计

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This study employs strong-motion data from the 1999 Chi-Chi earthquake, the 1999 Kocaeli earthquake, the 1999 Duzce earthquake, the 1995 Kobe earthquake, the 1994Northridge earthquake and the 1989 Loma Prieta earthquake to refine the relationship among critical acceleration (A_c), Arias intensity (I_a), and Newmark displacement (D_n). The results reveal that, as expected, logD_n is proportional to logIawhenAc is large. AsAc gets smaller however, the linearity becomes less. Wealso found that logD_n is proportional to A_c, and that the linearity is very stable through all I_a values. These features arecommonto all six sets of data. Therefore,we add a third termin addition to the Jibson's formwhich covers the aforementioned problem, and propose a new form for the relationship among I_a, A_c and D_n. Two alternative forms were tested using each of the six data sets, before a final form was selected. The final analyses grouped the data into a worldwide data set and a Taiwanese data set. Coefficients for the selected formwere derived from regression with the data, and two final empirical formulas, one for global, the other for local, proposed. Site conditions are also considered in this study with empirical formulas being developed for soil and rock sites, respectively. The estimation error is smaller and the goodness of fit is higher for both the local soil-site and rock-site formulas. Since landslides are more likely to occur on hillsides, the rock site formula may be more applicable for the landslide cases, whereas the soil site formula should be used for side slope of landfills.
机译:本研究采用了1999年集集地震,1999年科贾埃利地震,1999年杜兹采地震,1995年神户地震,1994年北岭地震和1989年洛马普里埃塔地震的强运动数据,以完善临界加速度(A_c)之间的关系,咏叹调强度(I_a)和纽马克位移(D_n)。结果表明,正如预期的那样,logD_n与logIawhenAc成正比。然而,随着AcAc变小,线性度变小。我们还发现logD_n与A_c成正比,并且线性度在所有I_a值中都非常稳定。这些功能是所有六组数据所共有的。因此,除了涵盖上述问题的吉布森形式外,我们还增加了第三项,并为I_a,A_c和D_n之间的关系提出了一种新形式。在选择最终表格之前,使用六个数据集分别测试了两种其他表格。最终分析将数据分为全球数据集和台湾数据集。所选形式的系数是通过对数据的回归得出的,并提出了两个最终的经验公式,一个是整体的,另一个是局部的。在这项研究中还考虑了场地条件,分别针对土壤和岩石场地开发了经验公式。对于本地土-场地和岩-场地公式,估计误差较小,拟合优度较高。由于山坡更可能发生滑坡,因此岩石位置公式可能更适用于滑坡情况,而土壤位置公式应用于垃圾填埋场的边坡。

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