胡志明市1区分布的砂土液化潜力评价

Hung V. Nguyen, S. Bui, Nu Thi Nguyen, Luan Nhat Vo, C. Vo, Dat Tuan Nguyen
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引用次数: 0

摘要

沙子的液化并不是一种罕见的地质现象。当它发生时,它会对人们造成很大的伤害。然而,胡志明市1区尽管是胡志明市的主要经济和政治区域,许多不同负荷的建筑和地铁线路已经和将要重建,但液化潜力尚未得到评估。基于不同地面加速度峰值情景下的标准贯入试验(SPT),对胡志明1区amSQ13海相更新世砂岩性复合体砂的液化潜力进行了研究。研究结果表明,当最大地加速度amax = 0.0848 g时,该区域很少有点发生液化。而当峰值加速度增大时,即amax= 0.1 g和amax= 0.15 g时,分别有8%和68%的测点出现液化。研究还表明,当深度为20m左右时,在amax = 0.1 g和amax = 0.15 g时,1区仍有液化的可能。研究结果可为研究人员和城市空间规划提供参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of liquefaction potential of sand distributed in the 1 District, Ho Chi Minh city
Liquefaction of sand is not a rare geological phenomenon. When it happens, it causes great damage to people. However, 1 District, Ho Chi Minh city where despite being a leading economic and political zone of Ho Chi Minh city, where many buildings with different loads and metro lines have been and will be rebuilt, but liquefaction potential has not been assessed. This paper presents a study on liquefaction potential of sand belonging to the Pleistocene sand lithological complex of marine origin on amSQ13 in 1 District, Ho Chi Minh based on standard penetration test (SPT) with different peak ground acceleration scenarios. Research results show that, when the peak ground acceleration amax = 0.0848 g, few points in this area occur liquefaction. However, when peak ground acceleration increased, specifically amax = 0.1 g and amax= 0.15 g, there were 8% and 68% of the survey points in the area where liquefaction occurred, respectively. The study also shows that, with a depth of about 20m, liquefaction in 1 District is still possible with amax = 0.1 g and amax = 0.15 g. The research results contribute to additional references for researchers and urban spatial planning in this area.
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