Show/Hide Menu
Hide/Show Apps
Logout
Türkçe
Türkçe
Search
Search
Login
Login
OpenMETU
OpenMETU
About
About
Open Science Policy
Open Science Policy
Open Access Guideline
Open Access Guideline
Postgraduate Thesis Guideline
Postgraduate Thesis Guideline
Communities & Collections
Communities & Collections
Help
Help
Frequently Asked Questions
Frequently Asked Questions
Guides
Guides
Thesis submission
Thesis submission
MS without thesis term project submission
MS without thesis term project submission
Publication submission with DOI
Publication submission with DOI
Publication submission
Publication submission
Supporting Information
Supporting Information
General Information
General Information
Copyright, Embargo and License
Copyright, Embargo and License
Contact us
Contact us
An overview of local site effects and the associated building damage in Adapazari during the 17 August 1999 Izmit earthquake
Date
2002-02-01
Author
Bakır, Bahadır Sadık
Sucuoğlu, Haluk
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
279
views
0
downloads
Cite This
Two major earthquakes occurred in Turkey along the North Anatolian fault in 1999. The first one, which occurred on 17 August 1999, had a moment magnitude of 7.4 and ruptured the 140-km segment of the fault in the Marmara region. Adapazari, a city with a population of 190,000, which is mostly located on a deep alluvial basin in the near field of the ruptured fault, was among the worst-affected urban areas in the earthquake-affected region. The distribution of damage over the city was highly nonuniform, indicating the variability of the ground response to the strong motion. Five- to six-story buildings located over deep alluvial soils were most adversely affected by the earthquake. Geotechnical characteristics of the alluvial basin of Adapazari are evaluated using the deep and shallow borehole Iogs and the measured parameters from the field and laboratory. This data is used for developing representative one-dimensional site-response models for various depths of alluvium and for liquefaction assessment in saturated surface soils. Recorded data from several aftershocks are utilized for model calibration. The results of soil-response studies are found to be highly Correlated with the general trends in the intensity and distribution of building damage. Based on in situ tests, soil liquefaction is determined to have occurred extensively in Adapazari which is in conformity with the postearthquake observations of widespread liquefaction-induced foundation displacements. Evidently, liquefied soil layers served as passive isolation mechanism for numerous buildings, some of which were subjected to excessive foundation displacements of various forms without signs of significant structural damage.
Subject Keywords
Geochemistry and Petrology
,
Geophysics
URI
https://hdl.handle.net/11511/36786
Journal
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
DOI
https://doi.org/10.1785/0120000819
Collections
Department of Civil Engineering, Article
Suggestions
OpenMETU
Core
A critical examination of near-field accelerograms from the sea of Marmara region earthquakes
Akkar, S; Gulkan, P (Seismological Society of America (SSA), 2002-02-01)
In 1999, Turkey was struck by two major earthquakes that occurred 86 days apart on the North Anatolian Fault system. Both earthquakes had right-lateral strike-slip mechanisms with moment magnitudes greater than 7. The number of strong-motion records obtained from the Kocaeli earthquake (17 August 1999, M-w 7.4) was 34. The second event, designated as the Bolu-Duzce earthquake (12 November 1999, M-w 7.2), triggered 20 instruments. Among the records that we have from these earthquakes, seven are from near-sou...
The 20th July 2017 Bodrum-Kos Tsunami Field Survey
Dogan, Gozde Guney; Annunziato, Alessandro; Papadopoulos, Gerassimos A.; GÜLER, HASAN GÖKHAN; Yalçıner, Ahmet Cevdet; Cakir, Tarik Eray; Sozdinler, Ceren Ozer; ULUTAŞ, ERGİN; Arikawa, Taro; Süzen, Mehmet Lütfi; Guler, Isikhan; Probst, Pamela; Kanoğlu, Utku; Synolakis, Costas (Springer Science and Business Media LLC, 2019-07-01)
The July 20, 2017 Bodrum-Kos Earthquake caused tsunami wave motions and damage in the south of Bodrum Peninsula, Turkey, and on Kos Island, Greece. Immediately after the earthquake, we conducted several post-tsunami field surveys including interviews in coastal zones impacted by the tsunami, i.e., the coastlines of Bodrum Peninsula, Karaada Islet and Akyaka Town in Gokova Bay, Turkey, and eastern Kos Island, Greece. We present observations and measurements to document the variation of the tsunami effects al...
The Chios, Greece Earthquake of 23 July 1949: Seismological Reassessment and Tsunami Investigations
Melis, Nikolaos S.; Okal, Emile A.; Synolakis, Costas E.; Kalogeras, Ioannis S.; Kanoğlu, Utku (Springer Science and Business Media LLC, 2020-03-01)
We present a modern seismological reassessment of the Chios earthquake of 23 July 1949, one of the largest in the Central Aegean Sea. We relocate the event to the basin separating Chios and Lesvos, and confirm a normal faulting mechanism generally comparable to that of the recent Lesvos earthquake located at the Northern end of that basin. The seismic moment obtained from mantle surface waves, M-0=7x10(26) dyn cm, makes it second only to the 1956 Amorgos earthquake. We compile all available macroseismic dat...
Stochastic Strong Ground Motion Simulation of the 12 November 1999 Duzce (Turkey) Earthquake Using a Dynamic Corner Frequency Approach
Ugurhan, Beliz; Askan Gündoğan, Ayşegül (Seismological Society of America (SSA), 2010-08-01)
On 12 November 1999, only three months after the 17 August 1999 Kocaeli earthquake (M(w) 7: 4), an earthquake of Mw 7: 1 occurred immediately to the east of the Kocaeli rupture in northwestern Turkey resulting in extensive structural damage in the city of Duzce and its surrounding area. It was reported to be a right-lateral strike slip event on the previously unbroken segment of the North Anatolian fault zone with a north-dipping fault plane. This paper presents stochastic finite-fault simulation of near-fi...
A 3000-Year Record of Ground-Rupturing Earthquakes along the Central North Anatolian Fault near Lake Ladik, Turkey
Fraser, Jeff; Pigati, J. S.; Hubert-Ferrari, Aurelia; Vanneste, Krıs; Avşar, Ulaş; Altinok, S. (Seismological Society of America (SSA), 2009-10-01)
The North Anatolian fault (NAF) is a similar to 1500 km long, arcuate, dextral strike-slip fault zone in northern Turkey that extends from the Karliova triple junction to the Aegean Sea. East of Bolu, the fault zone exhibits evidence of a sequence of large (M-w > 7) earthquakes that occurred during the twentieth century that displayed a migrating earthquake sequence from east to west. Prolonged human occupation in this region provides an extensive, but not exhaustive, historical record of large earthquakes ...
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
B. S. Bakır and H. Sucuoğlu, “An overview of local site effects and the associated building damage in Adapazari during the 17 August 1999 Izmit earthquake,”
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA
, pp. 509–526, 2002, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/36786.