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Seismic vulnerability indices of ground for Degirmendere (Kocaeli Province, Turkey)

机译:Degirmendere(土耳其考卡利省)的地面地震易损性指数

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It is well known that the mechanical and physical properties of subsoil layers as well as poor construction practices play an important role in determining the level of structural damage sustained from earthquakes. Thus, sufficient knowledge of these properties is essential for estimating the weak points of a region. The ground vulnerability index (K-g), an indicator of the weak points of a region, also has a substantial importance role in mitigating earthquake hazards in multidisciplinary studies. In this context, we have used engineering basement shear wave velocity (v(s30)), fundamental frequencies and peak amplitude values of the horizontal-to-vertical ratio (H/V) to calculate K-g values for the study area (Kocaeli Province, Turkey). Structural damage was investigated after the August 17, 1999 Kocaeli (M-w=7.4) Earthquake and compared with the calculated K-g values. The results indicate that the K-g values decrease towards the southern part of the study area, which is in good agreement with damage distribution from this earthquake. K-g values of 10 appear to be indicative of the most vulnerable areas in the study area. Structures built along the coastlines in Deirmendere area were the mostly severely damaged or collapsed entirely; we found that the subsoil beneath them have high K-g values of between 10 and 25 In contrast, K-g values in the southern districts, which sustained little or no damage, are relatively low (K-g10). In our study, the K-g values and soil types showed good agreement. Potential vulnerable areas also have poor subsoil conditions. Therefore, it could be important to consider these results for the future planning and designing of urban areas. These results could also be used as a rapid way to detect potential vulnerable areas before the occurrence of a destructive earthquake.
机译:众所周知,地下土壤层的机械和物理特性以及不良的施工实践在确定地震造成的结构破坏程度方面起着重要作用。因此,对这些特性的充分了解对于估算区域的薄弱点至关重要。地面脆弱性指数(K-g),是该地区薄弱环节的指标,在​​减轻多学科研究的地震危险中也具有重要作用。在这种情况下,我们使用了工程地下室横波速度(v(s30)),基频和水平与垂直比(H / V)的峰值幅度值来计算研究区域(Kocaeli Province,火鸡)。在1999年8月17日科贾埃利(M-w = 7.4)地震后调查了结构破坏,并将其与计算出的K-g值进行了比较。结果表明,K-g值在研究区域的南部逐渐降低,这与这次地震造成的破坏分布非常吻合。 K-g值> 10似乎表明研究区域中最脆弱的区域。代尔门德莱地区沿海岸线建造的建筑物大部分受到严重破坏或完全倒塌;我们发现它们下面的地下土壤具有较高的K-g值,介于10到25之间。相比之下,南部地区的K-g值相对较低(K-g <10),该值几乎没有或根本没有受到破坏。在我们的研究中,K-g值与土壤类型显示出良好的一致性。潜在的脆弱地区的土壤条件也很差。因此,考虑这些结果对于将来的城市规划和设计可能很重要。这些结果还可以用作在破坏性地震发生之前检测潜在脆弱区域的快速方法。

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