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EARTHQUAKE-INDUCED LANDSLIDE STABILITY ANALYSIS OF THE LAS COLINAS LANDSLIDE IN EL SALVADOR

机译:萨尔瓦多州拉斯科林纳斯滑坡的地震诱发滑坡稳定性分析

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摘要

The January 13, 2001 earthquake (M7.6) off the coast of El Salvador triggered widespread damaging landslides in many parts of the country. The Las Colinas landslide, located in Balsamo Ridge west of San Salvador, caused the greatest loss of life in a single location from the earthquake. The pre-earthquake and post-earthquake seismic stability analysis of the Las Colinas slope is studied using the limit equilibrium and finite element methods in this paper. The safety factor of the pre-earthquake slope was likely over 1.50 based on the low groundwater level, which was noted by local residents prior to the January 13 earthquake. The slope failed as the horizontal earthquake coefficient, kc, reached between 0.18g and 0.31g depending on the failure analysis methods (i.e. circle and trial surface methods) and the low soil strength assumed. The safety factor of the post-earthquake slope falls in a range from 1.851 at low water saturation to 1.337 when fully saturated. As compared with the pre-earthquake slope, the stability is about 8 percent higher for the post-earthquake slope.
机译:萨尔瓦多沿海地区2001年1月13日的地震(M7.6)引发了该国许多地区的广泛破坏性滑坡。位于圣萨尔瓦多以西的Balsamo Ridge的Las Colinas滑坡在地震中单个地点造成了最大的生命损失。本文采用极限平衡法和有限元方法研究了拉斯科利纳斯山坡地震前和震后的稳定性。基于低地下水位,地震前斜坡的安全系数可能超过1.50,这是1月13日地震前当地居民注意到的。当水平地震系数kc达到0.18g至0.31g之间时,边坡会失效,具体取决于失效分析方法(即圆形法和试验面法)和假定的低土壤强度。地震后斜坡的安全系数在低水饱和度时的1.851到完全饱和时的1.337的范围内。与地震前的坡度相比,地震后的坡度的稳定性大约高8%。

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