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dc.contributor.authorTopal, Tamer
dc.contributor.authorAkin, Muge
dc.contributor.authorDoyuran, Vedat
dc.date.accessioned2021-08-04T07:04:18Z
dc.date.available2021-08-04T07:04:18Z
dc.date.issued2017en_US
dc.identifier.isbn978-3-319-53498-5
dc.identifier.isbn978-3-319-53497-8
dc.identifier.urihttps //doi.org/10.1007/978-3-319-53498-5_32
dc.identifier.urihttps://hdl.handle.net/20.500.12573/901
dc.description.abstractLandslide is a natural process of the earth's surface, inevitably resulting from gravity with many triggering factors such as rainfalls, earthquakes, slope steepening, removal of vegetation, etc. The most frequent landslide-triggering mechanism is water from intense rainfall or human-based sources. The wide ranges of landslides and the complexity and variability of their interactions with the environment are the key points of a landslide investigation. The rate of the movement is the main factor of high property damages. On 16th of March in 2006, a rapid landslide occurred in Goynuklu village in Bursa, Turkey. The properties were inevitably damaged after the failure. The triggering factors of the failure mechanism and the properties of the landslide were investigated to specify proper remedial measures at the site. The geotechnical investigations including surface and subsurface studies were performed to determine the extent of the landslide and its sliding surface accurately. Within the framework of the geotechnical investigations, the inclinometer measurements were also recorded after drilling boreholes. Besides, a number of trial pits were excavated for evaluating the shallow sliding surfaces. Samples taken from the boreholes and trial pits were tested in the laboratory to obtain the soil class and the distribution of the grain size of the soil layers as well. The field tests including the hydraulic effect on the soil layers were also resolved by means of in situ permeability tests. Based on the data obtained, the characteristics and mechanism of the landslide were analyzed. The landslide occurred on a translational sliding surface in Neogene sediments including non-stratified sandstone-siltstone-claystone layers and a landfill site in a residential area. The shear strength characteristics of the sliding surface were calculated by back-analyses.en_US
dc.description.sponsorshipce Meeting4th World Landslide Forum LocationLjubljana, SLOVENIA DateMAY 29-JUN 02, 2017 SponsorsInt Consortium Landslides; Int Programme Landslides, Global Promot Comm; Geol Survey Slovenia Ljubljana; Univ Ljubljana; Republ Slovenia, Minist Environm & Spatial Planning; Republic Slovenia, Minist Infrastructure; Slovenian Natl Platform Disaster Risk Reduct; Int Programme Landslides; Slovenian Chamber Engineers; Int Assoc Hydrogeologists Slovene Comm; Water Management Soc Slovenia; Geomorphol Assoc Slovenia; Inst Water Republ Slovenia; Slovenian Geol Soc; Slovenian Geotechn Soc; IHP UNESCO, Slovenian Natl Comm; Slovenian Assoc Geodesy & Geophysen_US
dc.language.isoengen_US
dc.publisherSPRINGER INTERNATIONAL PUBLISHING AGGEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLANDen_US
dc.relation.isversionof10.1007/978-3-319-53498-5_32en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectTurkeyen_US
dc.subjectGoynuklu-Bursaen_US
dc.subjectGeotechnical investigationen_US
dc.subjectTranslational slideen_US
dc.subjectLandslideen_US
dc.titleLandslide Investigation of a Residential Area in Goynuklu Village, Bursa (Turkey)en_US
dc.typeconferenceObjecten_US
dc.contributor.departmentAGÜ, Mühendislik Fakültesi, İnşaat Mühendisliği Bölümüen_US
dc.identifier.volume281en_US
dc.identifier.endpage288en_US
dc.relation.journalADVANCING CULTURE OF LIVING WITH LANDSLIDES, VOL 2: ADVANCES IN LANDSLIDE SCIENCEen_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US


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