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Reseach Article

A Matlab based GUI Application in Hydro seismicity of the Koyna – Warna Region, India

by J. Pavan Kumar, D. V. Ramana, R. K. Chadha
International Journal of Computer Applications
Foundation of Computer Science (FCS), NY, USA
Volume 52 - Number 10
Year of Publication: 2012
Authors: J. Pavan Kumar, D. V. Ramana, R. K. Chadha
10.5120/8241-1522

J. Pavan Kumar, D. V. Ramana, R. K. Chadha . A Matlab based GUI Application in Hydro seismicity of the Koyna – Warna Region, India. International Journal of Computer Applications. 52, 10 ( August 2012), 38-43. DOI=10.5120/8241-1522

@article{ 10.5120/8241-1522,
author = { J. Pavan Kumar, D. V. Ramana, R. K. Chadha },
title = { A Matlab based GUI Application in Hydro seismicity of the Koyna – Warna Region, India },
journal = { International Journal of Computer Applications },
issue_date = { August 2012 },
volume = { 52 },
number = { 10 },
month = { August },
year = { 2012 },
issn = { 0975-8887 },
pages = { 38-43 },
numpages = {9},
url = { https://ijcaonline.org/archives/volume52/number10/8241-1522/ },
doi = { 10.5120/8241-1522 },
publisher = {Foundation of Computer Science (FCS), NY, USA},
address = {New York, USA}
}
%0 Journal Article
%1 2024-02-06T20:51:56.711642+05:30
%A J. Pavan Kumar
%A D. V. Ramana
%A R. K. Chadha
%T A Matlab based GUI Application in Hydro seismicity of the Koyna – Warna Region, India
%J International Journal of Computer Applications
%@ 0975-8887
%V 52
%N 10
%P 38-43
%D 2012
%I Foundation of Computer Science (FCS), NY, USA
Abstract

Hydroseismicity was proposed to explain the occurrence of intraplate earthquakes in regions. Koyna - Warna region one of the reservoir triggered seismicity zone in India, which is an example of intraplate earthquake region. The seismicity is continuing after 45 years of impoundment of the Koyna reservoir in 1961 and 25 years of impoundment of Warna reservoir in 1985. The excess of previous maximum water level, the annual rise of water level in the reservoirs and filling rate of these reservoirs are some of the important factors in increasing the pore pressure. In this study, we used the daily changes in the water levels in both the reservoirs and calculated the pore pressure from starting of the impoundment of the reservoir up to 2008. We also studied the pore pressure changes with depth for various values of hydraulic diffusivity. An automatic formulation has been developed in Matlab for computing and plotting the pore pressure history.

References
  1. Ahlvin, R. G. and Ulery, H. H. (1962), Tabulated values for determining the complete pattern of stresses, strains, and deflections beneath a uniform circular load on a homogeneous half space, Highw. Res. Board Bull. 342, 1–13.
  2. Chadha, R. K. , Kumpel, H. -J. , and Shekar, M. (2008), Reservoir Triggered Seismicity (RTS) and well water level response in the Koyna-Warna region, India, Tectonophysics 456, 94–102.
  3. Chen, L. and Talwani, P. (2001), Mechanism of initial seismicity following impoundment at the Monticello Reservoir, South Carolina, Bull. Seismol. Soc. Am. 91, 1582–1594.
  4. Cornet, F. H. and Yin, J. (1995), Analysis of induced seismicity for stress field determination and pore pressure mapping, Pure Appl. Geophys. 145, 677–700.
  5. Evans, K. F. , Genter, A. , and Sausse, J. (2005), Permeability creation and damage due to massive fluid injections into granite at 3. 5 km at Soultz: 1. Borehole observations, J. Geophys. Res. , B04203, doi: 10. 1029/2004JB003168.
  6. Gupta, H. K. (1992). Reservoir-Induced Earthquakes: Development in Geotechnical Engineering, 64, Elsevier, Netherlands, 364 pp.
  7. Gupta, H. K. (2002). A review of recent studies of triggered earthquakes by artificial water reservoirs with special emphasis on earthquakes in Koyna, India, Earth. Sci. Rev. 58, 279–310.
  8. Gupta, H. K. (2002). A review of recent studies of triggered earthquakes by artificial water reservoirs with special emphasis on earthquakes in Koyna, India, Earth Sci. Rev. 58 no. 3, 279–310.
  9. Gupta, H. K. , I. Radhakrishna, R. K. Chadha, H. -J. Kümpel, and G. Grecksch (2000). Pore pressure studies initiated in area of reservoir- induced earthquakes in India, Eos Trans. AGU 81, 145–151.
  10. Gupta, K. K. , 2001, Short – term earthquake forecasting may be feasible at Koyna, India, Tectonophysics, 353-357.
  11. Inmaculada Dura-Gomez and Pradeep Talwani, (2009), Hydromechanics of the Koyna–Warna Region, India, Pure Appl. Geophys.
  12. Kusala Rajendran & Pradeep Talwani, "The Role of Elastic, Undrained, and Drained Responses in Triggering Earthquakes at Monticello Reservoir, South Carolina," 82 Bull. Seismol. Soc. Am. 1867 (1992).
  13. Pandey, A. P. and CHADHA, R. K. (2003), Surface loading and triggered earthquakes in the Koyna-Warna region, western India, Phys. Earth Planet. Inter. 139, 207–223.
  14. Pandey, AP (2006) Triggering earthquakes of Koyna– Warna region. PhD thesis submitted to Osmania University, p 144
  15. Rajendran, K. and P. Talwani (1992). The role of undrained and drained responses in triggering earthquakes at Monticello Reservoir, South Carolina, Bull, Seism. Soc. Am. 82, 1867-1888.
  16. Rastogi, B. K. , Chadha, R. K. , Sarma, C. S. P. , Mandal, P. , Satyanarayana, H. V. S. , Raju, I. P. , Kumar, N. , Satyamurthy, C. , and Rao, A. N. (1997), Seismicity at Warna Reservoir (near Koyna) through 1995, Bull. Seismol. Soc. Am. 87, 1484–1494.
  17. Roeloffs, E. (1996). Poroelastic techniques in the study of earthquake related hydrologic phenomena, Adv. Geophys. 37, 135–195.
  18. Roeloffs, E. A. (1998). Persistent water level changes in a well near Parkfield, California, due to local and distant earthquakes. Journal of Geophysical Research 103, 869–889
  19. Simpson, D. (1986). Triggered earthquakes, Annu. Rev. Earth Planet. Sci. 14, 21–42.
  20. Talwani . P and S. Acree (1984/85). Pore pressure diffusion and the mechanism of reservoir-induced seismicity, Pure Appl. Geophys. 122, 947–965
  21. Talwani, P. (1995), Speculation on the causes of continuing seismicity near Koyna Reservoir, India, Pure Appl. Geophys. 145,167–174.
  22. Talwani, P. (1997). Seismotectonics of the Koyna-Warna area, India, Pure Appl. Geophys. 150, 511–550.
  23. Talwani, P. (2000). Seismogenic properties of the crust inferred from recent studies of reservoir-induced seismicity—Application to Koyna, Curr. Sci. India 79, 1327–1333.
  24. Talwani, P. and S. Acree (1984). Pore pressure diffusion and the mechanism of reservoir-induced seismicity. Pageophysics 122 (1984/85), 947–965.
  25. Talwani. P, Chen, L. , and Gahalaut, K. (2007), Seismogenic permeability, ks, J. Geophys. Res. 112, B07309, doi: 10. 1029/2006JB004665
  26. Witten, A. , 2004. A Matlab based three dimensional viewers. Computers & Geosciences 30, 693–703.
Index Terms

Computer Science
Information Sciences

Keywords

Koyna reservoir pore pressure diffusion Reservoir-induced seismicity stress memory strain hardening