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http://doi.org/10.22214/ijraset.2020.5214
May 2020
International Journal for Research in Applied Science & Engineering Technology (IJRASET) ISSN: 2321-9653; IC Value: 45.98; SJ Impact Factor: 7.429 Volume 8 Issue V May 2020- Available at www.ijraset.com
Computer Aided Analysis & Design of Structure in Tsunami Areas Arati G. Gawhale1, Prof. Hemant B. Dahake 2 1
P.G. Student, 2Assistant Professor, Department of Civil Engineering, G. H. Raisoni University, Amravati, Maharashtra, India
Abstract: The Indian Ocean tsunami on December 26, 2004 led to mass destruction of coastal communities with more than 3, 00000 fatalities, as well as severe damage to buildings, bridges and other infrastructure, causing serious socio-economic problems. Such a deadly mega-event made the coastal community aware of the need for preparedness against a primary shaking of the Earth and following the aftermath of the tsunami. The accident can be minimized with the correct early warning system and network of solid shelter and roads. Experience the recent tsunami of the Indian Ocean was new to the people of India. In the present study analysis of the structure is carried out in the tsunami area and compared with the structure without tsunami prone area. The different results in terms of the base shear, storey displacement, storey shear and stiffness is presented. Keywords: structure, tsunami, storey shear, displacement and stiffness I. INTRODUCTION The term tsunami comes from two Japanese words: ' tsu ', means a harbor, and ' us ', means wave. This is because these waves can create large jumps or fluctuations in coves or harbors that do not react to normal sea waves. In deep water, the tsunami is barely noticeable, but off the coast various mechanisms are causing a wave to grow over time by devastating consequences. The term tsunami was created by fishermen who returned to their ports to find the surrounding area devastated, although they were not aware of any wave in open water. The tsunami is caused by the rapid disturbances of the sea floor or water column above it, which either raise the sea surface above its normal level (normal case) or oppress it. This Tsunami produces a number of waves, or a wave train that extends outwards from the original area, until it either is dissipated or collides with the coastline. The physics of this spreading process is considered to be later. L: Wavelength (m) G: Water height (m) Ho: wave height in deep water (m) H: Wave height (m) d: Water depth (m) HR: Launch Wave (m) Ρ: Wave height (m) tsunami may be caused by: 1. Earthquakes 3. Volcanic eruption 2. Offsets 4. The meteorological combinations affecting these generating mechanisms often occur. As earthquakes are the most common cause of tsunamis, they will be developed in more detail. The present work deals with the structure with and without tsunami prone zone and the different results are obtained for the structure. II. REVIEW OF LITERATURE Based on the assessment of the repetition of periods of large earthquakes from past seismicity, convergence and seismological results, the possible future sources of the tsunami zone generating earthquakes in the Indian Ocean are identified along the subduction zone and compression zones. Through the movement of the Indian Plate in the northeast direction, the subduction zone is bounded on the north along the Himalayan region in conjunction with the continent-continent collision between the Indian and Eurasian plates, in the east along the Andaman-Sumatra Sunda Trench, where the Indian plate dove below the Burmese plate, as well as the subduction zone in the west along the Makran Coast, near Karachi, Pakistan. Thus, the Andaman-Sumatra and Makran subduction zone are two main sources in the Indian Ocean, where the earthquakes of magnitude 7.9 and above can occur, leading to a tsunami that can affect the east and West coast of India. (Chakha, 2006). Besides, Bangladesh-Myanmar coast has produced some well-documented tsunamis. Karachi-Kutch Coast Region also released some possible tsunamis. (Rasstgi and Jaiswal, 2006). The draft earthquake type along a subduction zone that causes vertical oceanic movement is usually tsunami related (Jaiswal ET Al., 2008-2). A minor tsunami can be obtained through a DIP integrated error along oceanic ridges. The distant tsunami hazard in the ocean Basin is a direct feature of seismic potential for extremely large events required to create a tsunami capable of exporting death and destroying distant shores. Studies show that the seismic moment of more than 7 x 1028 dyn.cm is required in this respect (Okal and Synolakis, 2008).
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International Journal for Research in Applied Science & Engineering Technology (IJRASET) ISSN: 2321-9653; IC Value: 45.98; SJ Impact Factor: 7.429 Volume 8 Issue V May 2020- Available at www.ijraset.com III.
MODELING
A. Building Description Table 1: Building Description Plane dimensions 12x18 m Total height of building 62.5 m Height of each storey 3.0m Height of parapet 1m Depth of foundation 1.5m Size of beams 300X500 MM size of columns 400X1200 MM Thickness of slab 125 mm Thickness of external walls 230 mm Thickness of internal walls 115mm Wind Speed 44/55 m/s Terrain Category 1 Class of Structure B Importance factor 1/1.08 Floor finishes 1.0 kN/m2 Live load at all floors 2 kN/m2 Grade of Concrete M30 Grade of Steel Fe500 Density of Concrete 25 kN/m3 Density of brick masonry 20 kN/m3
Figure 1: Plan of building The following models are prepared in this work: 1) 2) 3) 4)
Model I: 20 Storey Building without considering tsunami factor Model II: 20 Storey Building with considering tsunami factor Model III: 20 Storey Building with considering tsunami factor and with X Bracings at pheriphery Model IV: 20 Storey Building with considering tsunami factor and with X Bracings at Corners
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International Journal for Research in Applied Science & Engineering Technology (IJRASET) ISSN: 2321-9653; IC Value: 45.98; SJ Impact Factor: 7.429 Volume 8 Issue V May 2020- Available at www.ijraset.com IV.
RESULTS
A. Static Wind Analysis (X-Direction)
BASE SHEAR (X) IN KN 7000
BASE SHEAR
6000 5000 4000 3000 2000 1000 0 MOD I- Without Tsunami Factor
MOD II-With Tsunami Factor
MOD II-With MOD II-With Tsunami Factor and Tsunami Factor and with X Bracings at with X Bracings at pheriphery corners
Figure 2: Base Shear (X-Direction)
Storey Displacement-X (mm)
MOD I- Without Tsunami Factor 80 60 40 20 0
Storey Figure 3: Storey Displacement for Model-I
250 200 150 100 50 STOREY 1
STOREY 2
STOREY 3
STOREY 4
STOREY 5
STOREY 6
STOREY 7
STOREY 8
STOREY 9
STOREY 10
STOREY 11
STOREY 12
STOREY 13
STOREY 14
STOREY 15
STOREY 16
STOREY 17
STOREY 18
STOREY 19
0 STOREY 20
Storey Displacement-X (mm)
MOD II-With Tsunami Factor
Storey Figure 4: Storey Displacement for model-II
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International Journal for Research in Applied Science & Engineering Technology (IJRASET) ISSN: 2321-9653; IC Value: 45.98; SJ Impact Factor: 7.429 Volume 8 Issue V May 2020- Available at www.ijraset.com
MOD I- Without Tsunami Factor 5
Storey Drift - X (mm)
4.5 4 3.5 3 2.5 2 1.5 1 0.5 0
Storey Figure 5: Storey Drift for model-I
STOREY 1
STOREY 2
STOREY 3
STOREY 4
STOREY 5
STOREY 6
STOREY 7
STOREY 8
STOREY 9
STOREY 10
STOREY 11
STOREY 12
STOREY 13
STOREY 14
STOREY 15
STOREY 16
STOREY 17
STOREY 18
STOREY 19
10 9 8 7 6 5 4 3 2 1 0 STOREY 20
Storey Drift - X (mm)
MOD II-With Tsunami Factor and with X Bracings at corners
Storey Figure 6: Storey Drift for model-IV
MOD I- Without Tsunami Factor REINF. IN MM2
2194876
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Table 2: Steel consumption in columns MOD II-With Tsunami Factor MOD II-With Tsunami MOD II-With Tsunami Factor and with X Bracings at Factor and with X Bracings at corners pheriphery 3613956
2580832
2480054
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International Journal for Research in Applied Science & Engineering Technology (IJRASET) ISSN: 2321-9653; IC Value: 45.98; SJ Impact Factor: 7.429 Volume 8 Issue V May 2020- Available at www.ijraset.com
STEEL CONSUMPTION IN COLUMNS Reinforcement (mm2)
4000000 3500000 3000000 2500000 2000000 1500000 1000000 500000 0 MOD I- Without Tsunami Factor
MOD II-With Tsunami Factor
MOD II-With MOD II-With Tsunami Factor Tsunami Factor and with X and with X Bracings at Bracings at corners pheriphery
Figure 7: Steel consumption in columns for all models B.
Static Wind Analysis (Y-Direction)
Base Shear (KN)
Storey v/s Base Shear 3500 3000 2500 2000 1500 1000 500 0 MOD I- Without Tsunami Factor
MOD II-With Tsunami Factor
MOD II-With MOD II-With Tsunami Factor and Tsunami Factor and with X Bracings at with X Bracings at pheriphery corners
Figure 8: Base Shear (KN) for all storey
STOREY 1
STOREY 2
STOREY 3
STOREY 4
STOREY 5
STOREY 6
STOREY 7
STOREY 8
STOREY 9
STOREY 10
STOREY 11
STOREY 12
STOREY 13
STOREY 14
STOREY 15
STOREY 16
STOREY 17
STOREY 18
STOREY 19
35 30 25 20 15 10 5 0 STOREY 20
Storey Displacement-Y (mm)
MOD I- Without Tsunami Factor
Storey Figure 9: Storey Displacement for model-I
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International Journal for Research in Applied Science & Engineering Technology (IJRASET) ISSN: 2321-9653; IC Value: 45.98; SJ Impact Factor: 7.429 Volume 8 Issue V May 2020- Available at www.ijraset.com
80 60 40 20 STOREY 1
STOREY 2
STOREY 3
STOREY 4
STOREY 5
STOREY 6
STOREY 7
STOREY 8
STOREY 9
STOREY 10
STOREY 11
STOREY 12
STOREY 13
STOREY 14
STOREY 15
STOREY 16
STOREY 17
STOREY 18
STOREY 19
0 STOREY 20
Storey Displacement-Y (mm)
MOD II-With Tsunami Factor and with X Bracings at corners
Storey Figure 10: Storey Displacement for model-IV
Storey Drift - Y (mm)
MOD I- Without Tsunami Factor 3.5 3 2.5 2 1.5 1 0.5 0
Storey Figure 11: Storey Drift for model-I
Storey Drift - Y (mm)
MOD II-With Tsunami Factor 12 10 8 6 4 2 0
Storey Figure 12: Storey Drift for model-II
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International Journal for Research in Applied Science & Engineering Technology (IJRASET) ISSN: 2321-9653; IC Value: 45.98; SJ Impact Factor: 7.429 Volume 8 Issue V May 2020- Available at www.ijraset.com
Storey Displacement for Model-II Storey Displacement (mm)
250 200 150 100 50 0 1
2
3
4
5
6
7
8
9 10 11 12 13 14 15 16 17 18 19 20
Storey MOD II-With Tsunami Factor
MOD II-With Tsunami Factor
Figure 13: Storey Displacement for model-II
Storey Displacement for Model-IV Storey Displacement (mm)
160 140 120 100 80 60 40 20 0 1
2
3
4
5
6
7
8
9 10 11 12 13 14 15 16 17 18 19 20
Storey MOD II-With Tsunami Factor and with X Bracings at corners MOD II-With Tsunami Factor and with X Bracings at corners
Figure 14: Storey Displacement for model-IV V. From the above study following conclusions can be drawn: A. B. C. D. E.
CONCLUSION
Base shear is maximum for model-II as compared to other models Storey displacement is maximum in model II while it is minimum for model-I Storey drift is maximum in case of model-IV The maximum storey drift is found in storey 6 Steel consumption is minimum in model I when compared with other models
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International Journal for Research in Applied Science & Engineering Technology (IJRASET) ISSN: 2321-9653; IC Value: 45.98; SJ Impact Factor: 7.429 Volume 8 Issue V May 2020- Available at www.ijraset.com REFERENCES: [1]
Borrero J C, Synolakis C E, Fritz H, 2006, Northern Sumatra Field Survey after the December 2004 Great Sumatra Earthquake and Indian Ocean Tsunami, Earthquake Spectra, Vol.22, Nos.S3, pp. S93–S104. [2] Bryant E, (2001), Tsunami - The Underrated Hazard, Cambridge University Press, Cambridge, UK, 320 pp. [3] Chadha, R K, (2006). Collection of Papers by T. S. Murty, Tsunamigenic Sources in the Indian Ocean: Factors and Impact on the Indian Landmass [4] Clift P D, Kroon D, Gaedicke C, Craig J, (2002), The Techtonic and Climatic Evolution of the Arabian Sea Region, Geological Society, London, Special Publication, 195, pp.1-6. [5] Earthquake Engineering Field Investigation Team, (2006), The Indian Ocean Tsunami of 26 December 2004: Mission Findings in Sri Lanka and Thailand, Institution of Structural Engineers, London, UK. [6] Enet F and Grilli, S, (2005), Tsunami Landslide Generation: Modeling and Experiments, Ocean Waves Measurement and analysis, 5th International Symposium WAVES 2005, Madrid, Spain, pp. 88-97. [7] George Pararas-Carayannis, (2006), The Potential of Tsunami Generation Along the Makran Subduction Zone in the Northern Arabian Sea. Case Study: The Earthquake and Tsunami of November 28, 1945, Science of Tsunami Hazards, Vol-24, pp 358. [8] Imamura H, Roberton I, Preuss J, (2005), Development of Design Guide lines for Structures that Serve as Tsunami Vertical Evacuation Sites, Washington Division of Geology and Earth Resources Open File Report 2005-4. [9] Jaiswal R K, Rastogi B K, Murty T S, (2008), Tsunamigenic Sources in the Indian Ocean, Science of Tsunami Hazards, Vol. 27, No. 2, pp. 32-53. [10] Jaiswal R K, Singh A P, Rastogi B K, (2008), Simulation of the Arabian Sea Tsunami Propagation Generated Due to 1945 Makran Earthquake and Its Effect on Western Parts of Gujarat (India), Natural Hazards, vol. 48, pp. 245-258. [11] Jaiswal R K, Singh A P, Rastogi B K (2008). Simulation Of The Arabian Sea Tsunami Propagation Generated Due To 1945 Makran Earthquake And Its Effect On Western Parts Of Gujarat (India), Natural Hazards, 2008.
[12] Jordan B R, (2008), Tsunamis of the Arabian Peninsula a Guide of Historic Events, Science of Tsunami Hazards, Vol. 27, No. 1, page 31-46.
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