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SITE CLASSIFICATION PRACTICE IN SHALLOW BEDROCK REGIONS IN ASIA: COMPARISON OF RESPONSE SPECTRUM

机译:亚洲浅层基岩地区的现场分类实践:响应谱的比较

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Seismic site classifications are becoming very popular in Asia because of seismic microzonation studies. Seismic site classifications are used to represent seismic site effects and estimate the hazard parameters at soil surface. Most countries including Australia, China and India follow seismic site classification system similar to that in International Building Code (IBC), which is based on 30 m average shear wave velocity (SWV), Standard Penetration Test (SPT) N values and undrained shear strength (Anbazhagan et al, 2010). This simulates actual site amplification fairly accurately for cases wherein bedrock depth is near about 30m, but when bedrock depth is varying too much on shallow or deeper side, such classification is bound to render erroneous results. In the present study, focus is on developing and comparing response spectrum according to 30m classification and site response study considering earthquake in the study area with different depth of soil profiles. Soil profiles with SPT N and SWV are obtained from Anbazhagan et al. (2010). These sites are classified and response spectrum has been arrived according to site classification systems' recommendations in IBC, NEHRP and codes of India, Australia and China. Site response parameters of these sites are estimated by carrying out site specific response studies using SHAKE and earthquake reported in these regions. In the conclusion, comparison of responses obtained is made and a new site classification is proposed on basis of varying bedrock depth.
机译:由于地震微微型研究,地震位点分类在亚洲变得非常受欢迎。地震位点分类用于代表地震部位效应并估算土壤表面的危害参数。大多数国家,包括澳大利亚,中国和印度在国际建筑码(IBC)中遵循类似地震动现场分类系统,该系统是基于30米的平均剪力波速度(SWV),标准穿透试验(SPT)N值和不介绍的剪切强度(Anbazhagan等,2010)。这对壳体的情况进行了模拟了实际的现场放大器,以便在基岩深度接近约30米,但是当基岩深度在浅或更深的侧变化过多时,这种分类必然会呈现错误的结果。在本研究中,重点是根据30M分类和站点响应研究的响应谱进行响应谱,考虑到具有不同深度的土壤剖面的研究区域中的地震。具有SPT N和SWV的土壤分布是从Anbazhagan等人获得的。 (2010)。这些站点是分类的,并且根据IBC,澳大利亚和中国的IBC,Nehrp和Codes的网站分类系统建议已到达响应频谱。通过在这些地区报告的摇动和地震进行现场特异性响应研究,估计这些网站的网站响应参数。在结论中,制造所得响应的比较,并根据不同的基岩深度进行新的网站分类。

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