首页> 外文会议>7th U.S. National Conference on Earthquake Engineering >A COMPREHENSIVE SEISMIC VULNERABILITY AND LOSS EVALUATION OF THE STATE OF SOUTH CAROLINA USING HAZUS PART Ⅲ: LIQUEFACTION HAZARD
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A COMPREHENSIVE SEISMIC VULNERABILITY AND LOSS EVALUATION OF THE STATE OF SOUTH CAROLINA USING HAZUS PART Ⅲ: LIQUEFACTION HAZARD

机译:使用伤害的南卡罗来纳州状态的综合地震易损性和损失评估Ⅲ:液化危险

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The liquefaction hazard in South Carolina was evaluated as part of a statewide comprehensive seismic vulnerability and loss evaluation using HAZUS. HAZUS considers the potential for liquefaction (in terms of liquefaction-induced settlement and lateral flow) in assigning the potential for building damage. In the initial step in assigning liquefaction demand (in terms of cyclic stress ratio), reference rock datum motions were calculated for four earthquake scenarios. The events were a moment magnitude (M) 7.3 "1886 Charleston"-like earthquake, M 6.3 and M 5.3 events also from the Charleston seismic source, and a M 5.0 earthquake in Columbia. For each earthquake scenario and characteristic geologic profile, an average cyclic stress ratio within potentially liquefiable soil was calculated across the state at a 5 km x 5 km grid pattern. The characteristic profiles were developed using available subsurface and shear-wave velocity information, and considered a wide range of soil and rock conditions. The liquefaction resistance of soil in the representative profiles was determined based on shear-wave velocity and the clay/silt content of the soil. The results of the characterization and analyses indicate that greater amplification and liquefaction demand are experienced in the Charleston region than in other regions of South Carolina. The greater liquefaction demand, as well as the common presence of loose sand deposits, results in a greater risk of liquefaction in the Charleston region.
机译:使用HAZUS对南卡罗来纳州的液化危害进行了评估,作为全州范围内地震易损性和损失评估的一部分。 HAZUS在分配建筑物损坏的可能性时考虑了液化的可能性(就液化引起的沉降和侧向流动而言)。在分配液化需求的第一步(根据循环应力比)中,针对四种地震场景计算了参考岩石基准运动。这些事件是矩量级(M)7.3级“ 1886年查尔斯顿”地震,也来自查尔斯顿地震源的M 6.3和M 5.3级地震以及哥伦比亚的M 5.0级地震。对于每种地震场景和特征性地质剖面,在整个州以5 km x 5 km的网格模式计算了潜在液化土壤中的平均循环应力比。使用可用的地下和剪切波速度信息开发了特征剖面,并考虑了广泛的土壤和岩石条件。根据横波速度和土壤中的粘土/粉砂含量确定代表性剖面中土壤的抗液化性。表征和分析的结果表明,查尔斯顿地区比南卡罗来纳州其他地区经历了更大的扩增和液化需求。更大的液化需求以及松散的沙子沉积物的普遍存在,导致查尔斯顿地区更大的液化风险。

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