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Verification of Dynamic Behavior Modeling of Las Tórtolas Main Dam during 27F Chile Earthquake

机译:验证LasTórtolas主坝27F智利地震期间的动态行为建模

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Currently, the use of numerical dynamic analysis modeling for estimation of deformations in tailings deposits dams has increased, particularly in Chile in accordance with the requirements of country?s regulations (D.S. N° 248). Considering the relevance that these analyses have achieved, it is necessary to validate these models comparing their results with real measurements obtained for large earthquakes that have occurred in Chile in recent years. Because of this, the present study performs a three-dimensional dynamic analysis, using FLAC3D? software, of the main dam of Las Tórtolas tailings deposit, constructed with cycloned sand and located in the central zone of Chile, 45 km north from Santiago. Analysis was carried out for the geometry that presented the dam during the earthquake of February 27~(th), 2010 (27F Chile), magnitude Mw = 8.8 with its epicenter 360 km from the deposit. In the development of this study, information obtained from the geotechnical instrumentation that was operative at the time of the earthquake was used. Sands that constitute the dam were characterized by an extensive program of laboratory tests, which included among others: Consolidated Drained triaxial (CID), Consolidated Undrained (CIU and anisotropic), cyclic, small deformations triaxial and consolidation tests. To represent the behavior of this material an elasto-plastic constitutive model with a Mohr-Coulomb type failure criteria was used.At the date of the earthquake, the geotechnical instrumentation of dam included Casagrande piezometers, fiber optic piezometers and accelerometers, which allowed registering the seismic acceleration to which the dam was subjected and the variations of water table during the event.Residual post-earthquake deformations obtained by the model are compared with those induced by 27F Chile earthquake observed in the field.
机译:目前,在尾矿沉积物水坝使用数值动态分析建模为变形的估计有所增加,特别是在智利按照国家的要求?的规章(D.S. N°248)。考虑到这些分析所取得的相关性,有必要验证这些车型比较他们的结果与最近几年发生在智利的是大地震获得的实际测量。正因为如此,本研究中进行的三维动态分析,使用FLAC3D?软件,拉斯维加斯Tórtolas尾矿存款的主坝,构建了cycloned沙子和位于智利,圣地亚哥45公里北部的中心地带。分析进行,2010年2月27日〜(日),(27F智利)地震期间提出的坝的几何形状,大小MW = 8.8,其从存款震中360公里。在这项研究中的发展,从地质技术设备,这是在地震时手术中使用获得的信息。合并排水三轴(CID),固结不排水(CIU和各向异性),环状,小变形三轴和固结试验:通过实验室测试的广泛计划,其中包括除其他构成坝砂进行了表征。表示此材料与莫尔 - 库仑型破坏准则弹塑性构模型是used.At地震的日期的行为,大坝的土工仪器包括卡萨格兰德测压计,光纤压力计和加速度计,其允许注册地震加速度到该坝进行和水表的过程中由模型获得的event.Residual震后变形的变化与那些在该领域的观察到27F智利地震引起的比较。

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