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SITE RESPONSE ANALYSIS USING FORCED VIBRATION TESTS ON HYDRAULIC-FILLED SOIL DEPOSIT

机译:液压土层强迫振动试验的场地响应分析

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摘要

One of the most important and most commonly encountered problems in geotechnical earthquake engineering is the evaluation of a site response during an earthquake. The estimation of site response during an earthquake has been performed by using analytic and numerical site response analyses (SHAKE Analysis). 1 The natural frequency (resonant period) of a site is the most influential parameter in the estimation of site response during an earthquake. 2 The natural frequency of a site is usually estimated by numerical analysis or a simplified wave propagation equation. Engineering soil parameters used for the site response analysis (numerical analysis and simplified wave propagation equation) are acquired by in situ and laboratory tests; however, uncertainties in using the above parameters always exist. The uncertainties can be classified as follows: (1) disturbance of the soil specimen during the sampling procedure; (2) inherent experimental errors; and (3) obstacles in the in situ tests. Due to these uncertainties, if the natural frequency of the site can be estimated directly from in situ tests, it would be more reliable than numerical site response analysis results. However, over the past decades, surprisingly few attempts have been made to artificially represent an earthquake's motion by using such methods as a rotating mass or explosion. 3 '4 Thus, in this article, a spectral analysis method for direct estimation of the natural frequency of a site is executed at the experimental site by forced vibration tests. It uses the combination of a hydraulic hammer and dynamic compaction. Detailed site characterizations were also performed by using such in situ tests as a standard penetration test (SPT), a cone penetration test (CPT), and tests for shear wave velocity measurements. Soil particle motions, which were measured in a downhole receiver array as well as on the ground surface during the forced vibration tests, were used for estimating the natural frequencies of the experimental site, and they were compared with the results estimated by the analytic and the numerical analyses.
机译:在岩土地震工程中,最重要和最常遇到的问题之一是评估地震期间的现场响应。地震现场响应的估计是通过使用分析和数值现场响应分析(SHAKE分析)进行的。 1在估算地震期间的站点响应时,站点的自然频率(共振周期)是影响最大的参数。 2通常通过数值分析或简化的波传播方程估算站点的固有频率。通过现场测试和实验室测试获得用于场地响应分析的工程土壤参数(数值分析和简化的波传播方程);但是,在使用上述参数时始终存在不确定性。不确定性可以分类为:(1)采样过程中土壤样本的干扰; (2)固有的实验误差; (3)原位测试中的障碍。由于这些不确定因素,如果可以直接从现场测试中估算出站点的自然频率,则它会比数字站点响应分析结果更加可靠。然而,在过去的几十年中,出人意料的是,很少有人尝试通过使用诸如旋转质量或爆炸之类的方法来人为地代表地震的运动。 3'4因此,在本文中,通过强制振动测试在实验现场执行了用于直接估计现场自然频率的频谱分析方法。它结合了液压锤和动态压实功能。还通过使用诸如标准穿透测试(SPT),锥形穿透测试(CPT)和剪切波速度测量测试等原位测试来进行详细的位置表征。在强迫振动测试期间,在井下接收器阵列中以及在地面上测量的土壤颗粒运动被用于估计实验地点的固有频率,并将其与分析法和分析法估算的结果进行比较。数值分析。

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