Abstract

Earthquakes, when it comes to natural calamities, are characteristically devastating and pose serious threats to buildings in urban areas. Out of multiple seismic regions in the Himalayas, Bhutan Himalaya is one that reigns prominent. Bhutan has seen several moderate-sized earthquakes in the past century and various recent works show that a major earthquake like the 2015 Nepal earthquake is impending. The southwestern city of Bhutan, Phuentsholing is one of the most populated regions in the country and the present study aims to explore the area using geophysical methods (Multispectral Analysis of Surface Waves (MASW)) for understanding possibilities pertaining to infrastructural development. The work involved a geophysical study on eight different sites in the study region which fall under the local area plan of Phuentsholing City. The geophysical study helps to discern shear wave velocity which indicates the soil profile of a region along with possible seismic hazard during an earthquake event, essential for understanding the withstanding power of the infrastructure foundation. The acquired shear wave velocity by MASW indicates visco-elastic soil profile down to a depth of 22.2 m, and it ranged from 350 to 600 m/s. A site response analysis to understand the correlation of bedrock rigidness to the corresponding depth was conducted using EERA (Equivalent-linear Earthquake Site Response Analysis) software. The amplification factors are presented for each site and maximum amplification factors are highlighted. These results have led to a clear indication of how the bedrock characteristics influence the surface ground motion parameters for the corresponding structure period. The results infer that the future constructional activity in the city should not be limited to two- to five-story buildings as per present practice. Apart from it, a parametric study was initiated to uncover whatever effects rigid bedrock has upon hazard parameters for various depths of soil profile up to 30 m, 40 m, 60 m, 80 m, 100 m, 120 m, 140 m, 160 m, 180 m and 200 m from the ground surface. The overriding purpose of doing said parametric study is centered upon helping the stack holders who can use the data for future development. Such a study is the first of its kind for the Bhutan region, which suffers from the unavailability of national seismic code, and this is a preliminary step towards achieving it.

Highlights

  • The Himalayan region is considered as highly seismic, the Bhutan region has not faced an extreme earthquake (M > 6.5) for the past six decades [1]

  • There is a widespread belief that major earthquakes would not strike in Bhutan; it was reported that a major earthquake greater than a magnitude of 8 occurred in May 1713 which left in its wake widespread infrastructural damage and a staggering loss of human life

  • The Multispectral Analysis of Surface Waves (MASW) analysis in the present study indicates shear wave profile down to 22.2 m, peak ground acceleration (PGA) is constant at this level and depth of the bedrock is accounted for at 23 m

Read more

Summary

Introduction

The Himalayan region is considered as highly seismic, the Bhutan region has not faced an extreme earthquake (M > 6.5) for the past six decades [1]. Geological and geotechnical parameters affect the ground shaking intensity and influence the extent of damage resultant of an earthquake [19]. It may change the characteristics of surface seismic response, impairing present structures constructed over such grounds. The present study is a ground response analysis for bedrock characteristics using geophysical data and laboratory experiments on soil collected from the sites. Using the Equivalent-linear Earthquake Site Response Analysis (EERA) computer program as a tool for analysis, a layered visco-rigid soil profile is considered to analyze the effects of bedrock rigidness with changing depth.

Study Area
Methodology
Ground Response Analysis
Input Motion and Bedrock
Soil Properties
Static Properties
Dynamic Properties
Geophysical Site Exploration
CST football ground
Parametric Study
Conclusions
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.