Determination of the amplitude values with Nakamura (H/V) method and standard spectral ratio (Ssr) method at Ktu Campus

BildiriYalnız künye

Özet

Microtremor method used for engineering seismology is very important for determining of dynamic ground parameters and its variations. Method based on frequency of horizontal and vertical component microtremor records provides to quick and economical estimation of dynamic ground parameters. In this study, Nakamura (H/V) method and Standard Spectral Ratio (SSR) method have been applied to microtremor records taken with CMG-6TD three component broad band velocity seismometers in six profile with the aim of determining ground amplification of Karadeniz Technical University Campus area. The amplification maps of the study area are generated to the results of Nakamura (H/V) method and Standard Spectral Ratio (SSR) method and the results have been compared.

RDL Kalıcı Bağlantı (PID)
https://rdlopen.rawdatalibrary.net/r/gumushane/15775Resmi atıflarda kullanılan kalıcı adres
DOI
https://doi.org/10.3997/2214-4609.201414119Yayıncı resmi DOI adresi
Tam Kayıt
AlanDeğerDil
dc.contributor.authorBeker, Y.B.
dc.contributor.authorSayil, N.
dc.contributor.authorAkin, Ö.
dc.date.accessioned2026-10-22T10:24:31.264546476Z
dc.date.available2026-10-22T10:24:31.264546476Z
dc.date.issued2015
dc.description.abstractMicrotremor method used for engineering seismology is very important for determining of dynamic ground parameters and its variations. Method based on frequency of horizontal and vertical component microtremor records provides to quick and economical estimation of dynamic ground parameters. In this study, Nakamura (H/V) method and Standard Spectral Ratio (SSR) method have been applied to microtremor records taken with CMG-6TD three component broad band velocity seismometers in six profile with the aim of determining ground amplification of Karadeniz Technical University Campus area. The amplification maps of the study area are generated to the results of Nakamura (H/V) method and Standard Spectral Ratio (SSR) method and the results have been compared.
dc.identifier.doi10.3997/2214-4609.201414119
dc.identifier.isbn978-946282166-8
dc.identifier.scopus2-s2.0-85088752780
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/gumushane/15775
dc.language.isoen
dc.publisherEuropean Association of Geoscientists and Engineers, EAGE
dc.relation.conference8th Congress of the Balkan Geophysical Society, BGS 2015
dc.relation.ispartof8th Congress of the Balkan Geophysical Society, BGS 2015
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subject.otherSeismology
dc.subject.otherEconomical estimation
dc.subject.otherEngineering seismologies
dc.subject.otherGround parameters
dc.subject.otherMicrotremor method
dc.subject.otherSpectral ratios
dc.subject.otherTechnical universities
dc.subject.otherThree component
dc.subject.otherVertical component
dc.subject.otherFrequency estimation
dc.titleDetermination of the amplitude values with Nakamura (H/V) method and standard spectral ratio (Ssr) method at Ktu Campus
dc.typeConference Object
dspace.entity.typePublication
rdl.citation.openalex0
rdl.citation.scopus0
rdl.conference.date5 October 2015 through 8 October 2015
rdl.conference.placeChania
rdl.oa.statusclosed
rdl.source.indexSCOPUS