帕西格市地震液化易感性图

Ian Frederic P. Garcia, J. Go, Rio Jasmin D. Go, Paoala Beatrize B. Suspine, N. Concha
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引用次数: 5

摘要

利用马里基纳谷断裂系统的运动、平均断层滑动率和再现间隔来预测此次大地震的发生和特征。然而,这并不包括潜在的液化,这对于提供深刻的备灾计划和应急措施至关重要。因此,开发一种新的液化地图来解决这一问题至关重要。在这项研究中,Pasig市使用2000年至2016年每30个村的土壤调查报告进行了分析。该研究将利用半经验方法为帕西格市提供6.8、7.2和7.6级地震对应的液化易感性等高线图,从而使帕西格市受益。根据分析,在6.8级地震中,液化高度易感区占79%,最不易感区占21%。对于7.2级地震,84%的土地高度易感,16%的土地最不易感,而对于7.6级地震,87%的土地高度易感,13%的土地最不易感。因此,当预期的大地震发生时,帕西格市的绝大多数土壤预计会液化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Earthquake liquefaction susceptibility mapping of Pasig City
Marikina Valley fault system movements, average fault slip rates, and recurrence intervals were carried out to predict the occurrence and characteristics of the anticipated large-magnitude earthquake. This however does not include potential liquefaction that is essential in providing profound disaster preparedness plans and contingency measures. It is therefore vital to develop a novel liquefaction map to address this concern. In this study the City of Pasig was analysed using the Soil Investigation Reports from year 2000 to 2016 of each 30 barangays. The study will benefit the City of Pasig by providing liquefaction susceptability contour maps corresponding to earthquake magnitudes 6.8, 7.2 and 7.6 using Semi-Empirical Method. Based on the analysis, 79% are highly susceptible and 21% are least susceptible to liquefaction for earthquake magnitude of 6.8. Also there are 84% that are highly susceptible and 16% are least susceptible to liquefaction for earthquake magnitude of 7.2 while 87% are highly susceptible and 13% are least susceptible to liquefaction for earthquake magnitude of 7.6. A vast majority of the soils in the City of Pasig are therefore expected to liquefy when the expected large earthquake magnitude occur.
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