Published May 2018 | Version v1
Journal article

Back analysis of ground vibrations which cause cracks in buildings in residential areas Karakuyu (Dinar, Afyonkarahisar, Turkey)

  • 1. Süleyman Demirel University, Engineering Faculty, Geological Engineering Department (Turkey)

Description

The Karakuyu village (Dinar) is located in the south-western Turkey. Karakuyu settlement area suffered from ground vibration. There are two reasons for ground vibration in that area. One of them is earthquake and other is rock blasting. Geological structure and tectonics have great influence on vibrations in the area. An earthquake of magnitude Ms = 6.1 occurred on 1 October 1995, causing causalities and damage to buildings in Dinar and its vicinity. The earthquake forces during the main shock were amplified by poor dynamic characteristics of alluvial soils, thus resulting in damage to buildings. Limestone quarries are other source of ground vibration because of blasting. In this study, the source of vibration causing cracks in buildings in the Karakuyu residential area was investigated. Blasting at limestone quarries and past earthquake activities are analysed of ground vibrations which cause cracks in buildings. In the scope of this study, the source of the vibrations which cause the observed cracks in buildings were investigated using back analysis. As a result of the study, earthquake-induced vibrations on structural behaviour of buildings were found critical.

Additional details

Identifiers

Publishing Information

Journal Title
Natural Hazards
Journal Volume
92
Journal Issue
1
Journal Page Range
p. 497-509
ISSN
0921-030X

INIS

Country of Publication
Netherlands
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
50025379
Subject category
S58: GEOSCIENCES;
Descriptors DEI
BUILDINGS; CAUSALITY; CRACKS; DAMAGE; EARTHQUAKES; EXPLOSIVE FRACTURING; GEOLOGIC STRUCTURES; LIMESTONE; SOILS; TECTONICS; TURKEY
Descriptors DEC
ASIA; CARBONATE ROCKS; DEVELOPING COUNTRIES; FRACTURING; MIDDLE EAST; ROCKS; SEDIMENTARY ROCKS; SEISMIC EVENTS

Optional Information

Copyright
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