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Probabilistic Seismic Hazard Analysis for Low Seismicity Region

机译:低地震区概率地震危险性分析

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Critical facilities and structures such as nuclear and thermal power plants and dams, as well as the siting of new industry, require design ground motion data which are as accurate, homogeneous and complete as possible, so that hidden tectonic features may be revealed and seismic hazard assessed. Seismic hazard analysis is usually performed to obtain a characterization of the earthquake ground motion and liquefaction at a particular site. However, main interest is in the estimation of ground motion hazard, since it causes the largest economic loss in most earthquakes. Thus, the seismic hazard studies are carried out for estimating ground motion parameters expected to occur at bedrock levels at a particular site during strong earthquakes. Design earthquake selection process involves consideration of the seismic hazard at the site and the general response characteristics of the structure being analyzed considering the local site effects. Seismic hazard is commonly used to describe the severity of ground motion at a particular site without consideration of the consequences. In most situations the seismic hazard is uncertain, and is posed by the possible occurrence of earthquakes at more than one location; likewise, the sizes, or magnitudes of potentially damaging earthquakes. It is to be noted that the distance and magnitude of the causative fault have more effect on the nature of strong motion expected at a specific site. The methodologies for earthquake hazard analysis during the last few decades were developed primarily to assess seismic hazards of tectonically active areas (Cornell 1968; Der Kiureghian and Ang 1977; Wesnousky et al. 1984; McGuire 1995; Main 1995; Peter Tsai 2000; Rebez and Slejko 2000).
机译:关键设施和结构,例如核电厂,大坝以及新产业的选址,都要求设计的地震动数据要尽可能准确,均匀和完整,这样才能揭示隐藏的构造特征和地震危险评估。通常进行地震危险性分析以获得特定地点的地震地震动和液化的特征。但是,主要的兴趣在于估算地面运动的危害,因为它在大多数地震中造成最大的经济损失。因此,进行地震危险性研究是为了估计在强烈地震期间特定地点的基岩层预计会发生的地震动参数。设计地震的选择过程涉及考虑现场的地震危险,并考虑当地的现场影响来分析结构的一般响应特性。地震危险通常用于描述特定地点地面运动的严重性,而无需考虑后果。在大多数情况下,地震危险是不确定的,并且是由一个以上地点可能发生的地震引起的。同样,潜在破坏性地震的规模或大小。要注意的是,引起原因的断层的距离和大小对特定位置上预期的强运动的性质有更大的影响。在过去的几十年中,地震危险性分析的方法主要用于评估构造活动区的地震危险性(Cornell 1968; Der Kiureghian and Ang 1977; Wesnousky等人1984; McGuire 1995; Main 1995; Peter Tsai 2000; Rebez and Slejko 2000)。

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