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dc.contributor.authorDuman E.S.
dc.contributor.authorIkizler S.B.
dc.contributor.authorAngın Z.
dc.contributor.authorDemir G.
dc.date.accessioned2020-06-21T09:38:00Z
dc.date.available2020-06-21T09:38:00Z
dc.date.issued2014
dc.identifier.issn2005-307X
dc.identifier.urihttps://doi.org/10.12989/gae.2014.7.6.589
dc.identifier.urihttps://hdl.handle.net/20.500.12712/4853
dc.description.abstractThis study includes determination of liquefaction potential in Erzincan city center. Erzincan Province is situated within first-degree earthquake zone on earthquake map of Turkey. In this context, the earthquake scenarios were produced using the empirical expressions. Liquefaction potential for different earthquake magnitudes (6.0, 6.5, 7.0) were determined. Liquefaction potential was investigated using Standard Penetration Test (SPT). Liquefaction potential analyses are determined in two steps: geotechnical investigations and calculations. In the first steps, boreholes were drilled to obtain disturbed and undisturbed soil samples and SPT values were obtained. Laboratory tests were made to identify geotechnical properties of soil samples. In the second step, liquefaction potential analyses were examined using two methods, namely Seed and Idriss (1971), Iwasaki et al. (1981). The liquefaction potential broadly classified into three categories, namely non-liquefiable, marginally liquefiable and liquefiable regions. Additionally, the liquefaction potential index classified into four categories, namely non-liquefiable, low, high and very high liquefiable regions. In order to liquefaction analysis complete within a short time, MATLAB program were prepared. Following the analyses, liquefaction potential index is investigated by Iwasaki et al. (1982) methods. At the final stage of this study, liquefaction potential maps and liquefaction potential index maps of the all study area by using IDW (inverse distance weighted) interpolation method in Geostatistical Analyst Module of ArcGIS 10.0 Software were prepared for different earthquake magnitudes and different depths. The results of soil liquefaction potential were evaluated in ArcGIS to map the distributions of drillings with liquefaction potential. The maps showed that there is a spatial variability in the results obtained which made it difficult to clearly separate between regional areas of high or low potential to liquefy. However, this study indicates that the presence of ground water and sandy-silty soils increases the liquefaction potential with the seismic features of the region. © 2014 Techno-Press, Ltd.en_US
dc.language.isoengen_US
dc.publisherTechno Pressen_US
dc.relation.isversionof10.12989/gae.2014.7.6.589en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectEarthquakeen_US
dc.subjectGeostatistical analysisen_US
dc.subjectLiquefactionen_US
dc.subjectLiquefaction potentialen_US
dc.subjectLiquefaction potential indexen_US
dc.subjectStandard penetration testen_US
dc.titleAssessment of liquefaction potential of the Erzincan, Eastern Turkeyen_US
dc.typearticleen_US
dc.contributor.departmentOMÜen_US
dc.identifier.volume7en_US
dc.identifier.issue6en_US
dc.identifier.startpage589en_US
dc.identifier.endpage612en_US
dc.relation.journalGeomechanics and Engineeringen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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