One Dimensional Site Response Analysis of Liquefaction Potential along Coastal Area of Bengkulu City, Indonesia

L. Z. Mase
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引用次数: 8

Abstract

This paper presents one dimensional non-linear site response analysis of liquefaction potential caused by the 2000 and the 2007 earthquakes in coastal area of Bengkulu City, Bengkulu, Indonesia. Site investigations, including Standard Penetration Test (SPT) and shear wave velocity (VS) measurement, were conducted in three locations along the coastal area of Bengkulu City. Further, the site investigation data were used in simulation of one-dimensional non-linear site response analysis by applying the synthetic ground motions at bedrock. The results show that liquefaction could happen at 0 to 1.5 m deep. This was indicated by the excess pore water pressure ratio (ru) which exceeded one. At depth between 1.5 m and 20 m, the excess pore water pressure almost reached the initial effective stress decreasing the effective confinement pressure close to zero. The results also indicated that liquefaction is possible to occur in this depth range if a stronger earthquake occurs.
印尼明古鲁市沿海地区液化潜力的一维场地反应分析
本文对印尼明古鲁市沿海地区2000年和2007年地震液化潜力进行了一维非线性场地反应分析。在明古鲁市沿海地区的三个地点进行了现场调查,包括标准贯入试验(SPT)和剪切波速(VS)测量。此外,通过应用基岩的合成地震动,将现场调查数据用于模拟一维非线性场地反应分析。结果表明,液化可能发生在0至1.5米深。这通过超过1的过量孔隙水压力比(ru)来表示。在1.5米至20米的深度处,过量孔隙水压力几乎达到初始有效应力,使有效约束压力降至接近零。结果还表明,如果发生更强的地震,在这个深度范围内可能发生液化。
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15
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24 weeks
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