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Evaluation of site amplification, structural dynamic characteristics, and structural vulnerability rating of the city of Aqaba

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Abstract

The potential to destroy any structure during earthquakes depends on the structural design, vulnerability rating, percentage of structural elongation as compared with the natural quiet conditions, the dynamic characteristics of structure itself, as well as the dynamic characteristics of the site. Thus, factors related to the dynamic characteristics of structure and the dynamic characteristics of the site are necessary in the design of resistant structures against earthquakes. In this study, recordings of free oscillation were made directly on 18 selected structures in the urban city of Aqaba, which represent the structural culture of the city and the whole Jordan in general. Ground ambient vibration records were conducted at 18 nearby location at a few meters away from each structure. Records were conducted during the maximal cultural activities using three-component seismometer of 2 Hz free oscillation. Analytical results of records obtained on structures, has given the following equation: \( f = {18}/N \), where f, is the fundamental mode of structure and N, is the number of stories. All structural records were conducted at the top level of each structure except at Shmesani 4 and 7. Horizontal sensors were oriented with respect to the longitudinal and transverse direction of structural horizontal projection. Damping factors for each structural longitudinal and transverse fundamental mode were calculated based on the obtained FFT spectrums of each orientation using half-width band method. Analysis of obtained records on structures in Aqaba show that most of them are of short periodic structures except a few multi-story tall buildings. Most of the results obtained on structures refer to damping factors that range between 0.05 and 0.208. Mathematical relation derived from this study above, in addition to the actual calculated damping factor, refers to non-compliance with the standards of earthquake-resistant design. Results of ground records analysis indicate to the westward and north-westward decrease of dominant frequency relative to the eastern and southeastern part of the study area, where the crystalline granite bedrock is much shallower reflecting the actual condition of surface geology. Striking that the H/V amplification was relatively higher in the scope of areas where the thicknesses of soft surface deposits in the eastern and southeastern part are much shallower relative to the western and north-western part of the study area. This can be interpreted as a result of much higher impedance contrast in the eastern and southeastern part relative to the western and northwestern parts of the study area.

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References

  • Abou Karaki N (1987) Synthese et carte sismotectonique des pays de la bordure orientale de la Mediterranee: sismicite du systeme de failles du Jourdain-Mer Morte, These de Doctorat, U. Strasbourg, France, pp 417

  • Ambrayses NN, Melville CP, Adams RD (1994) The seismicity of Egypt Arabia and the Red Sea, a historical review. Cambridge University Press (ed), pp 181

  • Arieh E, Rotstein Y (1985) A note on the seismicity of Israel 1900–1982. Bull Seis Soc Am 75:881–887

    Google Scholar 

  • Ben Menahem A (1979) Earthquake catalog for the Middle East. Bollettino Geofisica Theorica Ed Applicata. Vol. XXI, 84:245–312

  • Bender F (1975) Geology of the Arabian Peninsula, Jordan. USGS. Geological Survey Professional Paper 560 - I

  • DeMets C, Gordon RG, Argus DF, Stein S (1994) Effects of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions. Geophys Res Let 21:2191–2194

    Article  Google Scholar 

  • Dunand F (2001) Determination de 1’amortissement et du centre de torsion des structure de genie civil par enregistrements de bruit de fond. Universite Joseph Fourier, Institut National Polytechnique de Grenoble

  • Fandi M (2002) “Expected Soil Dynamic Characteristics along the Eastern Shore of the Dead Sea”, NRA, JSO, Earthquakes in Jordan and Adjacent Areas, Bull No. 34, pp 30–46 (Arabic edition)

  • Fandi M (2004) “Surface Geology Dynamic Characteristics of the City of Maan”, NRA, JSO. Earthq Jordan Adjac Areas Bull 36:36–42 (Arabic edition)

    Google Scholar 

  • Gebel HGK (2009) “The Intricacy of Neolithic Rubble Layers. The Ba‘ja, Basta, and ‘Ain Rahub Evidence”, NEO-LITHICS 1/09, The Newsletter of Southwest Asian Neolithic Research, p 33–50

  • Giardini D, Jimenez MJ, and Grunthal G (2003) European – Mediterranean Seismic Hazard Map

  • Grafunkel Z, Ben Avraham Z (1996) The structure of the Dead Sea Basin. Tectonophysics 266(1–4):155–176

    Article  Google Scholar 

  • Grafunkel Z, Zak I, Freund R (1981) Active faulting in the Dead Sea rift. Tectonophysics 80:1–26

    Article  Google Scholar 

  • Justin F, Huchon P, Gaulier JM (1984) The Somalia plate and the Eastern Africa Rift System: present-day kinematics. Geophys J Int 116:637–654

    Article  Google Scholar 

  • Klinger Y (1999) Sismotectonique de la faille du Levant, These de Doctorat, Universite Louis Pasteur - Strasbourg I, France, pp 87

  • Korjenkov A, Schmidt K (2009) An Archaeoseismological Study at Tall Hujayrat al-Ghuzlan: Seismic Destruction of Chalcolithic and Early Bronze Age Structures. In: Lutfi Khalil - Klaus Schmidt (eds.) Prehistoric Aqaba I. Orient-Archäologie Band 23. 179–97. Rahden/Westf.: Verlag Marie Leidorf

  • Luft RW (1989) Comparisons among earthquake codes. EERI 5:767–789

    Google Scholar 

  • Nakamura Y (1989) A method for dynamic characteristics estimation of subsurface using microtremors on the ground surface. QR RTRI 30:25–33

    Google Scholar 

  • Nasser M, Tina M, Anil M (2004) A GIS-based assessment of liquefaction potential of the City of Aqaba, Jordan. Environ Eng Geosci X(4):297–320

    Google Scholar 

  • Quennell AM (1984) “The Western Arabian Rift System” The Geological Evolution of the Eastern Mediterranean. Dixon J, and Robertson A (ed) Geol. Soc. London, Spec. Publ., 17, 775–788

  • Rashdan M (1988) The regional geology of the Aqaba-Wade Araba area map sheets, 3049 III and 2949 II, Geol. Mapping Division Bull., NRA, Amman, Jordan, 7

  • Ross T, Tina M. Niemi, Thomas P (2007) “Structural damage from earthquake in the second-ninth centuries at the archaeological site of Aila in Aqaba, Jordan” Bulletin of the American Schools of Oriental Research © 2007

  • Ten Brink US Rybakov M, AL-Zoubi A, Hassouneh M, Frieslander U, Batayneh A, Goldshmidt V, Daud M, Rotstein Y, Hall J (1999) Anatomy of the Dead Sea transform: does it reflect continuous change in plate motion? Geology 27(10):887–890

    Article  Google Scholar 

  • Whitcomb D (1994) Ayla: Art and Industry in the Islamic Port of Aqaba: Special Publications. Special Publications, Oriental Institute, University of Chicago, Chicago, p 32

    Google Scholar 

  • Wood S (1991) Performance of reinforced concrete buildings during the 1985 Chile earthquake: implications for the design of structural walls. Earthquake Spectra 7:607–638

    Article  Google Scholar 

  • Zaslavsky Y, Shapira A (1994) Empirical determination of dynamic parameters of structures. In: Rutenberg A (ed) Earthquake engineering. Proceedings of the seventeenth Regional European seminar on earthquake engineering, Haifa, Israel, 5–10 September 1993

  • Zilberman E, Amit R, Porat N, Avner U (1998) Relocation of the epicenter of the 1068 earthquake in the Avrona Playa, southern Dead Sea rift, using paleoseismic and archeoseismic evidence. Abstract, 26th General Assembly of the European Seismological Commission, August 23–28, Tel-Aviv, Israel

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Acknowledgments

My sincere thanks to Dr. Maher Hijazin, the general director of the Natural Resources Authority; Engr. Darwish Jaser the director general/dministrator for Geological Survey, for their support and their encouragement. I would also like to thank the director of Geology, Mr. Bassam Al-Tarawneh for his support and encouragement during the implementation of the study. Great thanks and appreciations goes to Dr. Walter Hays and Dr. Ammar Shaker from the USA for their help and assistance in this study. Special thanks go to Engrs. Wajdi Al-Tameemy, special and sincere thanks to Engr. Nedal Al-Attiyat. Special thanks to the technician Mr. Ibrahim Mahasneh as well as Mr. Abdul Salam Ahazaymeh.

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Fandi, M., Alyazjeen, T. Evaluation of site amplification, structural dynamic characteristics, and structural vulnerability rating of the city of Aqaba. Arab J Geosci 6, 1465–1478 (2013). https://doi.org/10.1007/s12517-011-0444-y

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