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ANALYSIS OF SITE EFFECTS AND THEIR CORRELATION WITH DAMAGE DISTRIBUTION OBSERVED DURING THE COLIMA (MEXICO)EARTHQUAKE OF JANUARY 21, 2003

机译:2003年1月21日墨西哥(墨西哥)地震期间观测到的站点效应及其与损伤分布的相关性分析

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In order to evaluate the influence of ground condition on damage distribution in Villa de Alvarez town (Colima, Mexico) during the 2003 Colima earthquake ( MW=7.8), several geophysical surveys were carried out. The structure of shallow sedimentary materials and the depth of the basement have been estimated applying the Spatial Autocorrelation method (SPAC), using several regular pentagonal arrays with radii up to 25m. Seven S-wave velocity (VS) profiles have been inverted in Villa de Alvarez by using Rayleigh wave velocity dispersion curves for depths down to 30m. According to the local shallow structures obtained, we find clear lateral variations in the velocity structure for several urban zones that are correlated with different damage level.Microtremor measurements were recorded at 70 sites with a grid of about 100m x 100m interval across damaged area. The horizontal-to-vertical spectral ratios (HVSR) were determined in order to obtain the predominant period for each site. The predominant period range in the studied zone is about 0.1 . 0.6sec.Shorter predominant periods (0.1-0.2sec) were found in damaged zone whereas larger periods (greater than 0.4sec) were obtained in urban areas without damage. The site effects and their correlation with damage distribution on masonry structures observed during the 2003 Colima earthquake were very clear and remarkable. One of the main results has been that masonry houses with one or two storeys located on soils with dominant period around 0.15sec in Villa de Alvarez, showed the most serious damages.
机译:为了评估2003年科利马地震(MW = 7.8)期间地面条件对Villa de Alvarez镇(墨西哥科利马)的破坏分布的影响,进行了几次地球物理调查。浅层沉积物质的结构和地下室的深度已使用空间自相关方法(SPAC)进行了估算,该方法使用了几个半径最大为25m的规则五边形阵列。在Villa de Alvarez中,通过使用瑞利波速度色散曲线对深至30m的深度反演了七个S波速度(VS)剖面。根据获得的局部浅层结构,我们发现了几个与不同破坏程度相关的城市区域的速度结构存在明显的横向变化。在震荡区域的70个位置记录了微震测量结果,网格间隔约100m x 100m。确定水平与垂直光谱之比(HVSR),以获得每个站点的主要时段。研究区的主要周期范围约为0.1。 0.6秒。在受损区域发现更短的主要时期(0.1-0.2秒),而在没有破坏的城市地区获得更大的时期(大于0.4秒)。在2003年科利马地震中观察到的现场效应及其与砖石结构破坏分布的相关性非常清晰和显着。主要结果之一是,在Villa de Alvarez的土质房屋中,一层或两层的砖砌房屋的主宰期约为0.15秒,显示出最严重的破坏。

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