Analysis of Liquefaction Potential Based on The Grain Size Distribution of Soils and Cone Penetration Test (CPT) Data

Deo Pratama Prayitno, H. Artati
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Abstract

Liquefaction is a failure phenomenon in the soil layer which generally occurs due to cyclic loads from earthquakes. This study was conducted to determine the potential for liquefaction based on soil grain size distribution and CPT data in the UII Hospital area in Wijirejo Village, Bantul, DIY. Based on its geographical location, the Bantul district has a high earthquake potential because it is near an opak fault and is located in a subduction zone between the Indo-Australian Plate and the Eurasian plate. Along with this, there is urgency for this research. Analysis based on the grain size distribution of the soil was evaluated using the Tsuchida curve (1970). Analysis based on CPT data was evaluated using the Seed & Idris (1971) and IM Idriss & RW Boulanger (2008) equations to obtain a soil layer safety value, which was then used to predict the level of potential liquefaction with the LPI value using the Luna & Frost (1998) equation. Based on the grain size distribution using the Tsuchida curve (1970) in Wijirejo Village, the soil layer at a depth of 1 meter is dominated by sandy soil and silt, which has liquefaction potential. Based on CPT data, all sondir points have a very high liquefaction potential with consecutive LPI values 48,405; 52,160; 57,498; and 46,942 with a potential liquefaction zone depth of 0.20 to 13.20 meters from the ground level.
基于土壤粒度分布和圆锥贯入试验(CPT)数据的液化潜力分析
液化是土层的一种破坏现象,通常是由地震的循环荷载引起的。本研究基于Bantul Wijirejo村UII医院区域的土壤粒度分布和CPT数据来确定液化潜力。从地理位置来看,班图尔地区靠近不透明断层,处于印度-澳大利亚板块和欧亚板块之间的俯冲带,因此具有较高的地震潜力。与此同时,这项研究也迫在眉睫。采用土田曲线(1970)对土壤粒度分布进行分析。使用Seed & Idris(1971)和IM Idriss & RW Boulanger(2008)方程对基于CPT数据的分析进行评估,以获得土层安全值,然后使用Luna & Frost(1998)方程使用LPI值预测潜在液化水平。根据Tsuchida曲线(1970)在Wijirejo村的粒度分布,1 m深度的土层以沙土和粉土为主,具有液化潜力。基于CPT数据,所有sondir点具有非常高的液化潜力,连续LPI值为48,405;52160;57498;潜在液化区深度为0.20 ~ 13.20米,为46,942个。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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