Review of soil liquefaction characteristics during major earthquakes of the twenty-first century

Liquefaction, which can be defined as a loss of strength and stiffness in soils, is one of the major causes of damage to buildings and infrastructure during an earthquake. To overcome a lack of comprehensive analyses of seismically induced liquefaction, this study reviews the characteristics of liqu...

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Published inNatural hazards (Dordrecht) Vol. 65; no. 3; pp. 2375 - 2384
Main Authors Huang, Yu, Yu, Miao
Format Journal Article
LanguageEnglish
Published Dordrecht Springer Netherlands 01.02.2013
Springer
Springer Nature B.V
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Abstract Liquefaction, which can be defined as a loss of strength and stiffness in soils, is one of the major causes of damage to buildings and infrastructure during an earthquake. To overcome a lack of comprehensive analyses of seismically induced liquefaction, this study reviews the characteristics of liquefaction and its related damage to soils and foundations during earthquakes in the first part of the twenty-first century. Based on seismic data analysis, macroscopic phenomena of liquefaction (e.g., sand boiling, ground cracking, and lateral spread) are summarized, and several new phenomena related to earthquakes from the twenty-first century are highlighted, including liquefaction in areas with moderate seismic intensity, liquefaction of gravelly soils, liquefaction of deep-level sandy soils, re-liquefaction in aftershocks, liquid-like behavior of unsaturated sandy soils. Additionally, phenomena related to damage in soils and foundations induced by liquefaction are investigated and discussed.
AbstractList Liquefaction, which can be defined as a loss of strength and stiffness in soils, is one of the major causes of damage to buildings and infrastructure during an earthquake. To overcome a lack of comprehensive analyses of seismically induced liquefaction, this study reviews the characteristics of liquefaction and its related damage to soils and foundations during earthquakes in the first part of the twenty-first century. Based on seismic data analysis, macroscopic phenomena of liquefaction (e.g., sand boiling, ground cracking, and lateral spread) are summarized, and several new phenomena related to earthquakes from the twenty-first century are highlighted, including liquefaction in areas with moderate seismic intensity, liquefaction of gravelly soils, liquefaction of deep-level sandy soils, re-liquefaction in aftershocks, liquid-like behavior of unsaturated sandy soils. Additionally, phenomena related to damage in soils and foundations induced by liquefaction are investigated and discussed.
Liquefaction, which can be defined as a loss of strength and stiffness in soils, is one of the major causes of damage to buildings and infrastructure during an earthquake. To overcome a lack of comprehensive analyses of seismically induced liquefaction, this study reviews the characteristics of liquefaction and its related damage to soils and foundations during earthquakes in the first part of the twenty-first century. Based on seismic data analysis, macroscopic phenomena of liquefaction (e.g., sand boiling, ground cracking, and lateral spread) are summarized, and several new phenomena related to earthquakes from the twenty-first century are highlighted, including liquefaction in areas with moderate seismic intensity, liquefaction of gravelly soils, liquefaction of deep-level sandy soils, re-liquefaction in aftershocks, liquid-like behavior of unsaturated sandy soils. Additionally, phenomena related to damage in soils and foundations induced by liquefaction are investigated and discussed.[PUBLICATION ABSTRACT]
Liquefaction, which can be defined as a loss of strength and stiffness in soils, is one of the major causes of damage to buildings and infrastructure during an earthquake. To overcome a lack of comprehensive analyses of seismically induced liquefaction, this study reviews the characteristics of liquefaction and its related damage to soils and foundations during earthquakes in the first part of the twenty-first century. Based on seismic data analysis, macroscopic phenomena of liquefaction (e.g., sand boiling, ground cracking, and lateral spread) are summarized, and several new phenomena related to earthquakes from the twenty-first century are highlighted, including liquefaction in areas with moderate seismic intensity, liquefaction of gravelly soils, liquefaction of deep-level sandy soils, re-liquefaction in aftershocks, liquid-like behavior of unsaturated sandy soils. Additionally, phenomena related to damage in soils and foundations induced by liquefaction are investigated and discussed. Adapted from the source document.
Author Yu, Miao
Huang, Yu
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Issue 3
Keywords Lateral spread
Re-liquefaction
Deep soil liquefaction
Liquefaction-induced damage
Gravelly soil
Liquefaction characteristics
strength
foundations
liquefaction
stiffness
earthquakes
sand
natural disaster damages
boiling
buildings
aftershocks
seismic intensity
infrastructures
soils
Language English
License http://www.springer.com/tdm
CC BY 4.0
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Snippet Liquefaction, which can be defined as a loss of strength and stiffness in soils, is one of the major causes of damage to buildings and infrastructure during an...
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SubjectTerms Buildings
Civil Engineering
Damage
Earth and Environmental Science
Earth Sciences
Earth, ocean, space
Earthquakes
Earthquakes, seismology
Engineering and environment geology. Geothermics
Environmental Management
Environmental policy
Exact sciences and technology
Foundations
Geophysics/Geodesy
Geotechnical Engineering & Applied Earth Sciences
Hydrogeology
Infrastructure
Internal geophysics
Liquefaction
Natural Hazards
Natural hazards: prediction, damages, etc
Review Article
Sand
Sandy soils
Seismic activity
Seismic phenomena
Seismology
Soil (material)
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Title Review of soil liquefaction characteristics during major earthquakes of the twenty-first century
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