Earthquake-induced liquefaction in the coastal zone, Case of Martil city, Morocco
According to historical documents and Moroccan earthquakes catalogs, the coastal zone has suffered in the past from several earthquakes. Understanding how sedimentary basins respond to seismic-wave energy generated by earthquake events is a significant concern for seismic-hazard estimation and risk...
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doaj-8d003d98c0b8446baa43efcc94c188762021-08-09T08:00:12ZengEDP SciencesE3S Web of Conferences2267-12422021-01-012980100210.1051/e3sconf/202129801002e3sconf_iccr2021_01002Earthquake-induced liquefaction in the coastal zone, Case of Martil city, MoroccoEl Hilali Mohamed0Timoulali Youssef1Benyounes Taj2Ahniche Mohamed3El Bardai Rabie4Yattara Sahel5Earth Sciences Department, Scientific Institute, Mohammed V University in RabatEarth Sciences Department, Scientific Institute, Mohammed V University in RabatEarth Sciences Department, Scientific Institute, Mohammed V University in RabatGeoTechMed Laboratory, Tetouan Park: lot n°11GeoTechMed Laboratory, Tetouan Park: lot n°11Abdelmalk Essaadi University, Geology Department, Faculty of SciencesAccording to historical documents and Moroccan earthquakes catalogs, the coastal zone has suffered in the past from several earthquakes. Understanding how sedimentary basins respond to seismic-wave energy generated by earthquake events is a significant concern for seismic-hazard estimation and risk analysis. The main goal of this study is to determine the distribution of the natural frequency value (F), the amplification factor value (A), and the soil vulnerability index (Kg) were carried out as an indicator for liquefaction potential sites in the Martil city based on the microtremor measurements. Liquefaction assessment was done at 96 stations using the HVSR approach provided by Nakamura (1989). According to the analysis results, the predominant frequency values range from about 0.31 to 5.63 Hz, and the amplification factor values range from 3 to 15. Based on these parameters, the vulnerability index Kg is determined, which can be used as a parameter in calculating the liquefaction potential of an area. This study shows supporting evidence for the first time that the HVSR of microtremors can be an excellent alternative indicator for an area's potential for liquefaction.https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/74/e3sconf_iccr2021_01002.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
El Hilali Mohamed Timoulali Youssef Benyounes Taj Ahniche Mohamed El Bardai Rabie Yattara Sahel |
spellingShingle |
El Hilali Mohamed Timoulali Youssef Benyounes Taj Ahniche Mohamed El Bardai Rabie Yattara Sahel Earthquake-induced liquefaction in the coastal zone, Case of Martil city, Morocco E3S Web of Conferences |
author_facet |
El Hilali Mohamed Timoulali Youssef Benyounes Taj Ahniche Mohamed El Bardai Rabie Yattara Sahel |
author_sort |
El Hilali Mohamed |
title |
Earthquake-induced liquefaction in the coastal zone, Case of Martil city, Morocco |
title_short |
Earthquake-induced liquefaction in the coastal zone, Case of Martil city, Morocco |
title_full |
Earthquake-induced liquefaction in the coastal zone, Case of Martil city, Morocco |
title_fullStr |
Earthquake-induced liquefaction in the coastal zone, Case of Martil city, Morocco |
title_full_unstemmed |
Earthquake-induced liquefaction in the coastal zone, Case of Martil city, Morocco |
title_sort |
earthquake-induced liquefaction in the coastal zone, case of martil city, morocco |
publisher |
EDP Sciences |
series |
E3S Web of Conferences |
issn |
2267-1242 |
publishDate |
2021-01-01 |
description |
According to historical documents and Moroccan earthquakes catalogs, the coastal zone has suffered in the past from several earthquakes. Understanding how sedimentary basins respond to seismic-wave energy generated by earthquake events is a significant concern for seismic-hazard estimation and risk analysis. The main goal of this study is to determine the distribution of the natural frequency value (F), the amplification factor value (A), and the soil vulnerability index (Kg) were carried out as an indicator for liquefaction potential sites in the Martil city based on the microtremor measurements. Liquefaction assessment was done at 96 stations using the HVSR approach provided by Nakamura (1989). According to the analysis results, the predominant frequency values range from about 0.31 to 5.63 Hz, and the amplification factor values range from 3 to 15. Based on these parameters, the vulnerability index Kg is determined, which can be used as a parameter in calculating the liquefaction potential of an area. This study shows supporting evidence for the first time that the HVSR of microtremors can be an excellent alternative indicator for an area's potential for liquefaction. |
url |
https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/74/e3sconf_iccr2021_01002.pdf |
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