Determination of Vs_30 from existing geophysical investigation data

The Vs_30 refers to the velocity of transversal seismic waves in the upper earth crust (surface shallow depths) in the 0-30 m interval. This parameter reflects the integral ground properties and is used in almost all seismic hazard assessment software. The determination of Vs_30 is important, especi...

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Bibliographic Details
Published inEngineering Geology and Hydrogeology Vol. 36; no. 1; pp. 35 - 43
Main Authors Ranguelov, Boyko, Borg, Ruben Paul, Spassov, Edelvays, Shadiya, Fathimath, Frantzova, Antoaneta
Format Journal Article
LanguageEnglish
Published 06.02.2023
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Summary:The Vs_30 refers to the velocity of transversal seismic waves in the upper earth crust (surface shallow depths) in the 0-30 m interval. This parameter reflects the integral ground properties and is used in almost all seismic hazard assessment software. The determination of Vs_30 is important, especially in the case of urban territories, where in-situ measurements are very difficult and sometimes impossible due to dense urban areas, large anthropogenic noise and the need of expensive boreholes. The paper presents a methodology for extracting necessary data and information from archival sources, mainly geophysical measurements frequently executed for different prospecting purposes. The methodology for assessment of the integral values of Vs_30 is proposed for the definition of seismic hazard maps in Bulgaria. The methodology proposed, based primarily on archive data, represents an effective approach with significant results, especially for the intensive urbanized town territories located in high seismic areas.
ISSN:0204-7934
2738-6996
DOI:10.52321/igh.36.1.35