2020
DOI: 10.1007/s10518-020-00951-8
|View full text |Cite
|
Sign up to set email alerts
|

Technical guidelines for the assessment of earthquake induced liquefaction hazard at urban scale

Abstract: Microzonation for earthquake-induced liquefaction hazard is the subdivision of a territory at a municipal or submunicipal scale in areas characterized by the same probability of liquefaction manifestation for the occurrence of an earthquake of specified intensity.The liquefaction hazard at a site depends on the severity of expected ground shaking as well as on the susceptibility to liquefaction of that site. This in turn depends on geological, geomorphological, hydrogeological and geotechnical predisposing fac… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
8
0

Year Published

2020
2020
2024
2024

Publication Types

Select...
9

Relationship

1
8

Authors

Journals

citations
Cited by 20 publications
(8 citation statements)
references
References 43 publications
0
8
0
Order By: Relevance
“…Furthermore, the geotechnical data and the geophysical tests of Vs 30 , Nakamura and down-hole tests, allow to build a geological section of the subsoil of the city of Jama, being the interface depth between quaternary soils and tertiary rocks (as to the volcanic basement) at 90 m depth. The response of the terrain has been modeled using the linear equivalent model (analysis of effective stresses), while the response of the soil columns was subsequently calculated for each layer [44,45]. Furthermore, we have used information of stratigraphic units and shear-wave velocity as these data have been required in order to model the spectra for the city of Jama, including soil profiles and the ground motion data in accordance with the national regulations entitled NEC-11 (Norma Ecuatoriana de la Construcción, [46]).…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, the geotechnical data and the geophysical tests of Vs 30 , Nakamura and down-hole tests, allow to build a geological section of the subsoil of the city of Jama, being the interface depth between quaternary soils and tertiary rocks (as to the volcanic basement) at 90 m depth. The response of the terrain has been modeled using the linear equivalent model (analysis of effective stresses), while the response of the soil columns was subsequently calculated for each layer [44,45]. Furthermore, we have used information of stratigraphic units and shear-wave velocity as these data have been required in order to model the spectra for the city of Jama, including soil profiles and the ground motion data in accordance with the national regulations entitled NEC-11 (Norma Ecuatoriana de la Construcción, [46]).…”
Section: Introductionmentioning
confidence: 99%
“…6). The CPTu test was carried out within the LIQUEFACT project (Lai et al 2021) and the data of the SPT and laboratory tests and the velocity profile in the first 30 m (V s;30 ) were provided by the Sakarya Municipality. Fig.…”
Section: Soil Conditions and Ground Motionmentioning
confidence: 99%
“…Interest has thus grown in geospatial models, which are well suited for regional-scale applications, and which have recently been adopted by agencies in the European Union and United States (e.g. Allstadt et al, 2022; Lai et al, 2019). The US Geological Survey, for example, utilizes the seminal model of Zhu et al (2017) in scenario and post-event data products.…”
Section: Applications and Models That Should Not Be Ignoredmentioning
confidence: 99%