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Determination of mean shear wave velocity to 30 m depth for site classification using shallow depth shear wave velocity profile in Korea

机译:使用韩国浅深度剪切波速度剖面确定到30 m深度的平均剪切波速度以进行场地分类

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The mean shear wave velocity to a depth of 30 m (V(S)30), established in the western United States, is the current site classification criterion for determining the seismic design ground motion, taking site amplification potential account into. To evaluate V(S)30 at a site, a shear wave velocity (V-S) profile extending to a depth of at least 30 m must be acquired using in situ seismic tests. In many cases, however, the obtained V-S profile does not extend to a depth of 30 m due to unfavorable field conditions and limitations of testing techniques. In this study, V(S)30 and the mean shear wave velocity to depths less than 30 m (V(S)Ds) were calculated using V-S profiles of more than 30 m obtained by seismic tests at 72 sites in Korea, and the correlation between V(S)30 and V(S)Ds was drawn based on the computed mean V-S data. Additionally, a method for extrpolating the V-S profile from shallow depths to 30 m and bedrock was developed by building a shape curve based on the average data of all V-S profiles. These two methods of extrapolating V(S)30 from shallow V-S profiles, using V(S)Ds and a shape curve, resulted in less bias than the simple method in which the lowermost V-S value obtained is extended to the depth of 30 m. These two extrapolation methods are useful for V-S profiles extending to depths of at least 10 m. Furthermore, the shape curve method developed in this study may be useful in the western United States as well as in Korea. (C) 2015 Elsevier Ltd. All rights reserved.
机译:在美国西部建立的深度为30 m的平均剪切波速度(V(S)30)是确定地震设计地震动并考虑了场地放大潜力的当前场地分类标准。为了在现场评估V(S)30,必须使用原位地震测试获取延伸至至少30 m深度的剪切波速度(V-S)剖面。然而,在许多情况下,由于不利的现场条件和测试技术的限制,所获得的V-S剖面不会延伸到30 m的深度。在这项研究中,使用韩国72个地点的地震测试获得的30 m以上的VS剖面,计算了V(S)30和小于30 m的平均剪切波速度(V(S)Ds),并且V(S)30和V(S)Ds之间的相关性是基于计算得出的平均VS数据得出的。此外,通过基于所有V-S剖面的平均数据绘制形状曲线,开发了一种将V-S剖面从浅深度推至30 m以及基岩的方法。这两种使用V(S)D和形状曲线从浅V-S轮廓外推V(S)30的方法,与将获得的最低V-S值扩展到30 m的深度的简单方法相比,产生的偏差较小。这两种外推方法对于延伸至至少10 m深度的V-S剖面很有用。此外,在这项研究中开发的形状曲线方法可能在美国西部和韩国都有用。 (C)2015 Elsevier Ltd.保留所有权利。

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