基于N-SPT方法的苏拉威西马木朱市液化潜力评价

A. Arsyad, Andi Asti Nur Amaliyah, Sopian Paerong, A. R. Djamaluddin
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摘要

马穆朱是西苏拉威西省的首府,由于2021年1月15日发生的里氏6.2级地震,马穆朱的基础设施遭受了严重破坏。在那次事件中,有几个地方发现了液化现象,引发了建筑物的地基沉降。不幸的是,关于Mamuju地震危险性的信息仍然不足,而地震危险性评估迫在眉睫。因此,本研究旨在评估马木州市的液化潜力。通过一些钻孔和N-SPT测量进行了一系列岩土工程调查。对于液化评估,使用了估计CRRM=7.5的方法,包括NCEER(1996)、Vancouver Task Force(2007)、中国规范、日本公路桥规范、Shibata(1981)、Boulanger & Idriss(2014)、Cetin等人(2004)、Seed等人(1983)、Tokimatsu & Yoshimi(1983)和Kokusho等人(1983),而对CSR的估计则采用了简化方法(Seed, 1974)。结果表明,城市沿海地区液化易感程度较高。当地震加速度为0.367g(200年回复期地震)时,地表液化厚度为8 m;当地震加速度为0.414g(马木举断层7.0级确定性地震)时,地表液化厚度为10 ~ 16 m。液化引起的地面沉降是基于Ishihara & Yoshimi(1992)的方法计算的。计算发现,在每个假定地震加速度下,地面沉降可达18 ~ 50 cm, 31 ~ 71 cm。通过将经验方法预测的液化厚度和地面沉降值与现场实测值进行比较,验证了本文方法的有效性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Liquefaction Potential Assessment for the City of Mamuju Sulawesi by using N-SPT based methods
Mamuju is the capital city of West Sulawesi Province which has experienced severe damages along its infrastructures due to Majene Earthquake Mw. 6.2 on January 15th 2021. On that event, liquefaction phenomenon has been found on several places, triggering foundation settlements of buildings. Unfortunately, information on Mamuju’s earthquake hazard is still inadequate, while earthquake hazard assessment is urgently needed. Therefore, this study aims to assess liquefaction potential for the city of Mamuju. Serial geotechnical investigations were undertaken through a number of boreholes and N-SPT measurements.   For liquefaction assessment, methods of estimating CRRM=7.5 were used including NCEER (1996), Vancouver Task Force (2007), Chinese Code, Japanese Highway Bridge Code, Shibata (1981), Boulanger & Idriss (2014), Cetin et al. (2004), Seed et al. (1983), Tokimatsu & Yoshimi (1983), and Kokusho et al. (1983),  while estimation of CSR, the Simplified method (Seed, 1974) was employed. The results show that the coastal areas in the city has a high level of susceptibility to liquefaction. The liquefaction thickness of the ground would be 8 m deep for a 0.367g seismic acceleration (200 years return period earthquake), and 10 – 16 m for 0.414g seismic acceleration (deterministic Mw 7.0 of Fault Mamuju). Ground settlement induced by liquefaction was computed based on Ishihara & Yoshimi (1992) method. It was found that the ground settlement could be 18 – 50 cm, and 31 – 71 cm for each assumed seismic acceleration. The validity of the method used in this study was examined through the comparation of predictive liquefaction thickness and ground settlement based on the empiric methods with the measured ones in the field.
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