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首页> 外文期刊>Journal of earth system science >Determining the site effects of 23 October 2011 earthquake (Van province, Turkey) on the rural areas using HVSR microtremor method
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Determining the site effects of 23 October 2011 earthquake (Van province, Turkey) on the rural areas using HVSR microtremor method

机译:使用HVSR微震法确定2011年10月23日地震(土耳其范省)对农村地区的现场影响

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A magnitude of 7.1 Mw earthquake struck Van city on October 23, 2011. Although, construction practices of all rural housing units are similar in the region, the earthquake caused massive damage to villages located on soft soils in northern region of the city. In this study, the effects of soil conditions on damaged housing units were determined by conducting horizontal to vertical spectral ratios of microtremor (HVSR) measurements. The level of damage in the villages that are settled on lacustrine and stream sediments has verified that the damage correlates well with comparatively high HVSR peak period and HVSR peak amplitude values in the range of 0.2a€“1.6 s and 4a€“10, respectively. The HVSR peak period and HVSR peak amplitude levels on rock units are in the range of 0.1a€“0.2 s and 1.5a€“2, respectively. It is important to note that hillside effect is found to be another key factor that increased the level of damage to the housing units in some villages.
机译:2011年10月23日,范城发生了7.1兆瓦级地震。尽管该地区所有农村住房单位的建设方式都相似,但地震对该市北部软土地上的村庄造成了严重破坏。在这项研究中,土壤条件对受损房屋单元的影响是通过进行微震(HVSR)测量的水平与垂直光谱比来确定的。沉积在湖泊和河流沉积物上的村庄的破坏程度已证明,该破坏与较高的HVSR峰值周期和HVSR峰值幅度值(分别在0.2a” 1.6 s和4a”“ 10”的范围内有很好的相关性) 。岩石单元上的HVSR峰值周期和HVSR峰值幅度水平分别在0.1a±0.2 s和1.5a±2之间。重要的是要注意,发现山坡效应是增加某些村庄房屋单元损坏程度的另一个关键因素。

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