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dc.contributor.authorIlkisik, Osman Metin
dc.contributor.authorGurer, Aysan
dc.contributor.authorGÜRER, ÖMER FEYZİ
dc.contributor.authorVarli, Tunc Bahadir
dc.date.accessioned2021-03-04T07:43:46Z
dc.date.available2021-03-04T07:43:46Z
dc.date.issued2016
dc.identifier.citationGurer A., Varli T. B. , Ilkisik O. M. , GÜRER Ö. F. , "Electrical imaging of the geoenvironment around water infrastructures in Istanbul city", ENVIRONMENTAL EARTH SCIENCES, cilt.75, sa.23, 2016
dc.identifier.issn1866-6280
dc.identifier.otherav_5f90a8dc-d30f-4f15-b34d-b0e74a4bab3b
dc.identifier.othervv_1032021
dc.identifier.urihttp://hdl.handle.net/20.500.12627/66749
dc.identifier.urihttps://doi.org/10.1007/s12665-016-6254-5
dc.description.abstractSubsurface structures from two different districts of Istanbul, hosting waste and freshwater transmission lines, were imaged by geoelectrical method. The environmental impact on Kag. ithane-Terkos freshwater transmission line is one of the issues. That waterline underwent a substantial landslide damage. The previous site selection of Kag. ithane-Terkos line was only based on surface geological observations. Even though the pipeline was positioned away from the surface scarps of landslides, the pipes were damaged. To find out the reason, we made some vertical electrical sounding measurements using Schlumberger array in the region. We inverted the electrical sounding data using 2D inversion technique. The final geoelectrical images show main landslide failures, at about 10-30 m depth, which are overlain by debris with a resistivity value of with <6 Omega m. The geoelectrical findings reveal that a buried major failure surrounds the surface landslides behind. Consequently, the water infrastructure remains under the influence of landslide. Our second application site was the area of the Sazlidere tunnel, which will transfer wastewater, polluting Sazlidere dam, to the treatment plant. The geoelectrical images along Sazlidere tunnel route show resistive (<100 Omega m) and moderately conductive (<= 50 Omega m) structures along the tunnel axis, representing unaltered to highly weathered rocks, respectively. Furthermore, consecutive hidden fault zones which severely affect the construction process of the tunnel are detected and located.
dc.language.isoeng
dc.subjectTarımsal Bilimler
dc.subjectZiraat
dc.subjectToprak ve Bitki Besleme
dc.subjectToprak ve Su Muhafazası ve Amenajmanı
dc.subjectHavza Yönetimi
dc.subjectÇevre Mühendisliği
dc.subjectJeoloji Mühendisliği
dc.subjectMühendislik ve Teknoloji
dc.subjectSU KAYNAKLARI
dc.subjectJEOLOJİ
dc.subjectTemel Bilimler (SCI)
dc.subjectYerbilimleri
dc.subjectYER BİLİMİ, MULTİDİSİPLİNER
dc.subjectTarım ve Çevre Bilimleri (AGE)
dc.subjectÇevre / Ekoloji
dc.subjectÇEVRE BİLİMLERİ
dc.titleElectrical imaging of the geoenvironment around water infrastructures in Istanbul city
dc.typeMakale
dc.relation.journalENVIRONMENTAL EARTH SCIENCES
dc.contributor.departmentAffin Int , ,
dc.identifier.volume75
dc.identifier.issue23
dc.contributor.firstauthorID237393


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