首页> 外文会议>Asian conference on remote sensing;ACRS >DETERMINISTIC LANDSLIDE MODELING OF THE JULY 1990 EARTHQUAKE IN CARRANGLAN NUEVA ECIJA USING NEWMARK METHOD
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DETERMINISTIC LANDSLIDE MODELING OF THE JULY 1990 EARTHQUAKE IN CARRANGLAN NUEVA ECIJA USING NEWMARK METHOD

机译:基于Newmark方法的1990年7月卡兰格怒火山的确定性滑坡建模。

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Nueva Ecija, Philippines is one of the towns showing traces and evidence of faulting as a consequence of the devastating July 1990 earthquake in Central Luzon, thus many houses, infrastructures, and lives were affected. In this study, a deterministic landslide modeling using Newmark Method was executed in order to produce a more detailed attributes for landslide susceptibility classification. The geotechnical properties of rock were obtained using Slope Stability Probability Classification (SSPC) while the reconstituted soil samples had undergone Direct Shear Test. Three rock exposures show cohesion values of 20,170 Pa, 25,350 Pa, 11, 700 Pa, and friction angle values of 40.22°, 49.22°, and 24.43°. Two soil samples show cohesion values of 12, 944.78 Pa and 8,041 Pa, and friction angle values of 29.41° and 44.69°. The factor of safety, critical acceleration, and peak ground acceleration, was computed using the cohesion and friction angle as parameters, generating a slope stability model. In the output slope stability model, 42.92% of the area is categorized as unstable, 20.27% is slightly stable, 30.51% is moderately stable, and 5.85% of the area is stable. Compared to the output prepared by PHIVOLCS, the slope stability model generated showed a difference in the classification of the landslide susceptible areas in the vicinity. This study discusses the efficiency of a deterministic landslide modeling based on Newmark's sliding-block model and producing a more detailed landslide slope stability model.
机译:菲律宾新埃奇亚(Nueva Ecija)是1990年7月吕宋岛中部地震造成的断层痕迹和断层证据之一,因此许多房屋,基础设施和生活受到影响。在这项研究中,使用Newmark方法执行确定性滑坡建模,以便为滑坡敏感性分类提供更详细的属性。岩石的岩土特性是使用边坡稳定性概率分类法(SSPC)获得的,而重建后的土壤样品已通过了直接剪切试验。三种岩石暴露显示的内聚力值为20,170 Pa,25,350 Pa,11,700 Pa,摩擦角值为40.22°,49.22°和24.43°。两个土壤样品的内聚力值为12、944.78 Pa和8,041 Pa,摩擦角值为29.41°和44.69°。使用内聚力和摩擦角作为参数计算安全系数,临界加速度和地面峰值加速度,从而生成边坡稳定性模型。在输出斜率稳定性模型中,将42.92%的区域分类为不稳定,将20.27%的区域划分为轻微稳定,将30.51%的区域划分为中等稳定,而将5.85%的区域划分为稳定。与PHIVOLCS的输出相比,生成的边坡稳定性模型显示了附近滑坡易感区域的分类差异。这项研究讨论了基于纽马克(Newmark)滑块模型的确定性滑坡建模的效率,并产生了更详细的滑坡稳定性模型。

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