Open Access Open Access  Restricted Access Subscription Access

Tremors and built environment of Hyderabad, Telangana, India: safety of buildings using recorded ground motions


Affiliations
1 Earthquake Engineering Research Centre, International Institute of Information Technology, Hyderabad 500 032, India
2 International Institute of Information Technology, Hyderabad 500 032, India
 

Although the city of Hyderabad in Telangana, India lies in seismic zone II, low to medium intensity tremors that pose a serious concern towards safety of the built environment are not uncommon. One such series of tremors occurred during 13–20 October 2020, in the financial district of Hyderabad and created a panic situation due to perceivable shaking and jolts with loud sounds associ­ated with hydro-seismicity. To understand the safety of the city’s built environment, a study was conducted on low, medium and tall buildings using ground motions recorded at the International Institute of Information Technology (IIIT), Hyderabad, which is 2.3 km from the epicentre. The amplification of ground motion on the second floor of the Nilgiri Building in IIIT, Hyderabad was 1.2–2.3. The vibrations recorded on the ground floor of the Nilgiri Building were used to develop a site-specific response spectrum. This was further used to obtain the peak responses of the considered buildings through response spectrum analysis. The present study suggests that the low-rise buildings, mid-rise buildings and non-structural elements in high-rise buildings are under threat in the case of high-intensity earthquakes

Keywords

Built environment, ground motion, hydroseismicity, microtremors.
User
Notifications
Font Size

  • NGRI, Micro quakes hit Hyderabad’s financial district after floods. NGRI scientists set up seismic stations. CSIR-National Geophysical Research Institute, Hyderabad, 2020; https://www.csir.res.in/slider/micro-quakes-hit-hyderabads-financial-district-afterfloods-ngri-scientists-set-seismic
  • Rastogi, B. K., Rao, C. V. R. K., Chadha, R. K. and Gupta, H. K., Microearthquakes near Osmansagar reservoir, Hyderabad, India. Phys. Earth Planet. Inter., 1986, 44(2), 134–141; https://doi.org/ 10.1016/0031-9201(86)90039-7.
  • Guha, S. K. and Basu, P. C., Catalogue of earthquakes (M> = 3) in Peninsular India, Atomic Energy Regulatory Board, Mumbai, Report No. AERB-TD-CSE-1, AERB, Mumbai, 1993.
  • Srinagesh, D. et al., Seismicity studies in eastern Dharwar craton and neighbouring tectonic regions. J. Geol. Soc. India, 2015, 85, 419–430; https://doi.org/10.1007/s12594-015-0232-5.
  • Singh, A. P., Kumar, V. V. and Mishra, D. C., Subsurface geometry of Hyderabad granite pluton from gravity and magnetic anomalies and its role in the seismicity around Hyderabad. Curr. Sci., 2004, 86(4), 580–585; https://www.currentscience.ac.in/Downloads/article_id_086_04_0580_0586_0.pdf
  • Maheswari, K., Senthil Kumar, P., Mysaiah, D., Ratnamala, K., Sri Hari Rao, M. and Seshunarayana, T., Ground penetrating radar for groundwater exploration in granitic terrains: a case study from Hyderabad. J. Geol. Soc. India, 2013, 81, 781–790; https://doi.org/10.1007/s12594-013-0103-x
  • Himabindu, D. and Ramadass, G., Structural framework of the region in and around Hyderabad as inferred from satellite image analysis: implications for seismic activity. MAUSAM, 2004, 55(1), 214–218; https://metnet.imd.gov.in/mausamdocs/25518.pdf
  • Murty, C. V. R., Goswami, R., Vijayanarayanan, A. R., Pradeep Kumar, R. and Mehta, V. V., Introduction to earthquake protection of non-structural elements in buildings, Gujarat State Disaster Management Authority, Government of Gujarat, Gandhinagar, 2013; https://www.iitk.ac.in/nicee/IITK-GSDMA/NSE_002_31May2013.pdf
  • Murty, C. V. R. et al., Reinforced concrete structures. Earthq. Spectra, 2002, 18(1_suppl), 149–185; https://doi.org/10.1193/1.2803911.
  • Lizundia, B. et al., M 7.8 Gorkha, Nepal earthquake on April 25, 2015 and its aftershocks, EERI Learning From Earthquakes Program, Earthquake Engineering Research Institute, Oakland, California, 2016; https://www.eeri.org/what-we-offer/learning-from-earthquakes
  • Trifunac, M. D. and Brady, A. G., A study on the duration of strong earthquake ground motion. Bull. Seismol. Soc. Am., 1975, 65(3), 581–626; https://core.ac.uk/download/pdf/216195618.pdf
  • Newmark, N. M. and Hall, W. J., Earthquake Spectra and Design, Earthquake Engineering Research Institute Monograph Series, 1982.
  • Sudarshan, K. and Bhole, V., Chronology of micro earthquakes in the environs of Hyderabad: a historical perspective. Int. J. Basic Appl. Res., 2019, 9(3), 4–15; http://www.pragatipublication.com/assets/uploads/doc/15683-04-15.16341.pdf
  • Gangrade, B. K., Prasad, A. G. V., Kumar, M., Unnikrishnan, E. and Nagaraja, C., Seismicity of peninsular India and earthquaken catalogue based on Gauribidanur seismic array data. Bhabha Atomic Research Centre, Technical Report No. BARC/2012/E/005, BARC, Mumbai, 2012; https://inis.iaea.org/collection/NCLCollectionStore/_Public/43/066/43066296.pdf?r=1

Abstract Views: 367

PDF Views: 160




  • Tremors and built environment of Hyderabad, Telangana, India: safety of buildings using recorded ground motions

Abstract Views: 367  |  PDF Views: 160

Authors

Pulkit Dilip Velani
Earthquake Engineering Research Centre, International Institute of Information Technology, Hyderabad 500 032, India
Neelima Patnala
Earthquake Engineering Research Centre, International Institute of Information Technology, Hyderabad 500 032, India
Bharat Prakke
Earthquake Engineering Research Centre, International Institute of Information Technology, Hyderabad 500 032, India
S. L. N. Shastry
International Institute of Information Technology, Hyderabad 500 032, India
R. Pradeep Kumar
Earthquake Engineering Research Centre, International Institute of Information Technology, Hyderabad 500 032, India

Abstract


Although the city of Hyderabad in Telangana, India lies in seismic zone II, low to medium intensity tremors that pose a serious concern towards safety of the built environment are not uncommon. One such series of tremors occurred during 13–20 October 2020, in the financial district of Hyderabad and created a panic situation due to perceivable shaking and jolts with loud sounds associ­ated with hydro-seismicity. To understand the safety of the city’s built environment, a study was conducted on low, medium and tall buildings using ground motions recorded at the International Institute of Information Technology (IIIT), Hyderabad, which is 2.3 km from the epicentre. The amplification of ground motion on the second floor of the Nilgiri Building in IIIT, Hyderabad was 1.2–2.3. The vibrations recorded on the ground floor of the Nilgiri Building were used to develop a site-specific response spectrum. This was further used to obtain the peak responses of the considered buildings through response spectrum analysis. The present study suggests that the low-rise buildings, mid-rise buildings and non-structural elements in high-rise buildings are under threat in the case of high-intensity earthquakes

Keywords


Built environment, ground motion, hydroseismicity, microtremors.

References





DOI: https://doi.org/10.18520/cs%2Fv122%2Fi10%2F1174-1184