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Determination of seismic compression of sand subjected to two horizontal components of earthquake ground motions

机译:确定地震地震动两个水平分量作用下砂土的地震压缩

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The objective of this Technical Note is to investigate the ratio of seismic compression of sand subjected to two mutually perpendicular horizontal components of earthquake ground motions simultaneously to its counterpart for single component of horizontal motions. By using a verified, fully coupled and inelastic finite element procedure, sand specimens with various relative densities (Dr=45%, 60% and 100%) are subjected to each of the horizontal components of motion separately, and then simultaneously, with the vertical strains and corresponding ratio computed for each case. In total, 296 shallow crustal horizontal motions (i.e. 148 sets of horizontal motions) with various earthquake magnitudes, site to source distances, durations, and site conditions recorded in active tectonic regions are used in the analyses. The results showed that the ratio generally ranges from 1.52 to 2.32, and it increases with earthquake magnitude and relative density of sand but decreases with epicentral distance. These results can be used in conjunction with seismic compression correlations for single component of motion to estimate its counterpart for multiple components of motion, thereby increasing the accuracy in predicting the severity of seismic compression under multi-directional seismic motions.
机译:本技术说明的目的是研究同时受到两个相互垂直的地震地震动水平分量的砂的地震压缩与相对于水平运动的单一分量的砂的地震压缩的比率。通过使用经过验证的,完全耦合的非弹性有限元程序,使具有不同相对密度(Dr = 45%,60%和100%)的砂试样分别经受水平运动的各个分量,然后同时使其垂直运动。每种情况下计算的应变和相应比率。在分析中,总共使用了296个浅地壳水平运动(即148组水平运动),这些水平地震具有不同的地震震级,站点到震源的距离,持续时间以及在活动构造区域中记录的站点条件。结果表明,该比值一般在1.52〜2.32之间,随地震烈度和沙相对密度的增加而增大,但随震中距离的减小而减小。这些结果可以与单个运动分量的地震压缩相关性结合使用,以估计其与多个运动分量的对应关系,从而提高预测多方向地震运动下地震压缩严重性的准确性。

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