地震位移预测方法、程序、比较及应用

Tecnia Pub Date : 2023-06-06 DOI:10.21754/tecnia.v33i1.1335
Luis Felipe Rojas Gomez, Lesly Scarlet Ortiz Galindo, Jesús Andrés Cabrera Conislla
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引用次数: 0

摘要

边坡抗震设计的方法随着技术进步和岩土工程的发展而发展,从具有很大局限性的方法(如伪静态分析)到需要大量信息才能更好地了解土壤特性的严格方法(如动力分析)。本文介绍了简化地震位移方法的程序、比较和应用,这些方法分别是Newmark方法(1965年)、Makdisi&Seed方法(1978年)、Bray和Travasarou方法(2007年)以及Bray、Macedo和Travasaru方法(2018年)。这些简化地震位移的方法中的每一种都与一个解释滑动体行为的模型相关联,本文分析了该模型的刚性块模型、解耦模型和耦合模型。作为一个应用案例,显示了一个50米高的岩石和中心心墙的土坝,该土坝位于砂岩地层和夹杂页岩侵入体的冰碛沉积物中,作为1974年利马地震、2001年阿提克地震和地震的地震考虑因素。Pisco 2007,考虑到NS和EW方向。同样,对大坝中3根立柱的响应分析得出的断层表面的响应谱也被视为信息。采用Newmark(1965)、Makdisi&Seed(1978)、Bray和Travasarou(2007)以及Bray、Macedo和Travasaru(2018)的方法,获得了1至10cm的变形结果,根据其数量级,这些结果代表了大坝的稳定状态。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seismic displacement prediction methods, procedure, comparison and application
The methodology in the seismic design of slopes has evolved with technological advancement and the development of geotechnical engineering, methods with great limitations such as pseudostatic analysis to rigorous methods that require a lot of information for a better understanding of the behavior of the soil such as the dynamic analysis. This article develops the procedure, comparison and application of simplified earthquake-induced displacement methods, which are the Newmark method (1965), the Makdisi & Seed method (1978), the Bray and Travasarou method (2007), and the method of Bray, Macedo and Travasarou (2018). Each of these methods of simplified earthquake-induced displacements is associated with a model that explains the behavior of the sliding mass, of which the rigid block model, the decoupled model and the coupled model are analyzed in this article. As an applicative case, an earthen dam with rocky and central core 50 m high placed in sandstone strata and moraine deposits interspersed with shale intrusions is shown, as seismic consideration the Lima 1974 earthquake, the Attic 2001 earthquake and the earthquake were used. of Pisco 2007, considering both NS and EW directions. Likewise, the response spectrum on the fault surface, resulting from a response analysis to 3 columns in the dam, is considered as information. The methods of Newmark (1965), Makdisi & Seed (1978), Bray and Travasarou (2007), and Bray, Macedo and Travasarou (2018) were applied, obtaining deformation results between 1 to 10 cm that according to their order of magnitude represent a stable condition for the dam.
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