Abstract

Chile is one of most seismic countries in the world. In the past 100 years, more than 8 major seismic events occurred in Chile, with the coastal area of central Chile being one of the most affected Since 2007, nearly 2,306 earthquakes were recorded in this area with magnitudes varying between 1.9 and 6.9 in the Ritcher and Mercalli scales. The earthquakes’ impact on the engineering structures depends on several factors, such as: the depth of the wave, wave type, geomorphological aspects of the rock, and soil properties. Chile central region of is a very important economics area, but at the same time, very vulnerable. The cities existing on this area, are installed in coastal plains, limited by Coastal Mountains and Pacific Ocean. Most of the seismic activity episodes recorded by Nacional Seismological center (CSN) is on the ocean. The present research aims to identify the regions vulnerable to significant seismic activities based on the average shear wave velocity on the upper 30m (Vs30) and using Geographic Information Systems. The Vs30 values were measured by the United Stated Geological Service (USGS). This analysis is based on the topography, geological units classified by Chilean norms NCh433, NCh2369, and law decree 61/ 2011. The analysis indicated that last epicenter city, Cobquecura, is the low vulnerable area, considering high Vs30 values and low number of habitants. Cities as Concepción, Talcachuano, San Pedro de la Paz, Coronel y Hualpén are more vulnerable because low Vs30 values, and high population. This factor can be associated to river mouths and floodplains presents in this area.

Highlights

  • Chile is one of most seismic countries in the world, registering in 2017 a total of 8,094 earthquakes

  • The seismic impact to the surface can be measured by the secondary wave velocity of propagation on the first 30 meters of surface

  • This research analyzed the Vs30 values of eleven cities, based on United Stated Geological Service (USGS) data which were acquired by tectonic measurements

Read more

Summary

Introdution

Chile is one of most seismic countries in the world, registering in 2017 a total of 8,094 earthquakes. An 8.8 Mw earthquake with epicenter at Cobquecura in 2010 caused infrastructure damage mainly in coastal zone at central Chile [3] near the earthquake epicenter. In this area, the historical data recorded from 2006 to 2019 indicate increase in the number of daily small earthquakes (short period and magnitude less than 6.9 Mw) in the last thirteen years. The seismic impact to the surface can be measured by the secondary wave velocity of propagation on the first 30 meters of surface These values are related with capacity of wave propagation, expressed by material. The municipality of Talcahuano (one of the cities evaluated in this work) is recognized internationally for considering natural disasters problems [6, 7]

Seismic wave propagation
Antecedents
Study area
Historical seismic situation
Geomorphology
Seismic response
Results
Conclusions
Full Text
Published version (Free)

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