Abstract

The city of Banda Aceh is potentially exposed to a significant seismic hazard of seismic site amplification. Estimation of seismic site amplification of the city is urgently required for any mitigation efforts as the city is founded on a thick, soft layer. This study aims to estimate seismic site amplification of Banda Aceh's soil. Analytical models have demonstrated that they can simulate reasonably well the seismic ground motions amplification. The most widely used model is the equivalent linear approach. The approach computes the ground response of horizontally layered soil deposits subjected to transient and vertically propagating shear waves through a one-dimensional soil column. As aforementioned, this study focuses on Banda Aceh-Indonesia which is founded on thick alluvium. Three actual historical time histories and three developed sub-surface models were used to estimate the seismic site amplification of Banda Aceh's soft soil. The used time histories are of 2012 M8.1 Simeulue earthquake, 2013 M6.0 Mane-Geumpang earthquake and 2013 M6.2 Bener Meriah earthquake. Three sub-surface models of three separate sites across the city of Banda Aceh were developed. The site response analysis results reveal the ground motions amplification of Banda Aceh's soils of up to 4.3. Thus, applying the seismic site amplification for structural design at Banda Aceh can be further works.

Highlights

  • In term of seismicity, the city of Banda Aceh and its surrounding areas is mainly generated by the northnortheast oriented convergence of the Indo-Australian plate toward the Eurasian plate with the rate of collision from about 40 -60 mm per year [1]

  • This study examines the impact of three historical seismic events on estimating seismic site amplification in the case of Banda Aceh - Indonesia

  • The results of the site response analysis of this study suggest a fundamental frequency of 0.6 Hz for all investigated sites, which can significantly amplify the medium-rise to high-rise buildings throughout the city

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Summary

Introduction

The city of Banda Aceh and its surrounding areas is mainly generated by the northnortheast oriented convergence of the Indo-Australian plate toward the Eurasian plate with the rate of collision from about 40 -60 mm per year [1] Banda Aceh is potentially exposed to an additional and significant seismic hazard along the Great Sumatran Fault (GSF) Understanding Banda Aceh's ground surface behaviour is essential for city infrastructure plan

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