ground response analyses in kathmandu valley
TRANSCRIPT
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GROUND RESPONSEANALYSES IN KATHMANDU
VALLEY
Dipendra Gautam
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OUTLINES
Introduction
Geology of Nepal
Geology of Kathmandu Valley
Seismicity
Research Objectives
Methodology
Results
Discussions
Conclusion
Research Horizon
Acknowledgements
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INTRODUCTION
Effects of Earthquakes:
Ground Shaking
Structural Hazards
Liquefaction
Landslides
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INTRODUCTION
Ground Shaking
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INTRODUCTION
Structural hazard
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INTRODUCTION
Landslide
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INTRODUCTION
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Site Effects
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Ampli tude r(t)= source signal e(t)*
distance from source p(t)* local site
effects s(t)
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INTRODUCTION
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Seismic Hazard Map of
Nepal ( After DMG)
Kathmandu
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INTRODUCTION
Site Effects are important
1985 Mexico City earthquake (Mw=8.1) 1989 Loma Prieta earthquake (Mw=7.1)
NEPAL: An earthquake prone area…!
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GEOLOGY OF NEPAL
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Kathmandu
After Uprety and Le Fort, 1999
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GEOLOGY OF KATHMANDU
VALLEY
6/29/2014 12After DMG
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GEOLOGICAL CROSS SECTION
OF KATHMANDU VALLEY
6/29/2014 13After Sakai, 2001
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SEISMICITY
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Rupture zones of large Himalayan earthquakes since 1800 (After
Bilham et. al., 2001, modified by Feldl, 2005)
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SEISMICITY
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Intense micro-seismicity monitored between 1994 and 2005 (
after DMG, 2006)
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RESEARCH OBJECTIVES
Work out equivalent linear site response
analyses of soft sediment deposit of Kathmandu
valley
Comparison of computed parameters with the
damage pattern of 1934 Bihar-Nepal earthquake
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METHODOLOGY
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BOREHOLE LOCATIONS
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INPUT MOTION
(Uttarkashi earthquake) TimeHistory
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Response spectra
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RESULTS
PEAK HORIZONTAL ACCELERATION
PEAK SPECTRAL ACCELERATION
AMPLIFICATION FACTOR
PREDOMINANT PERIOD
PEAK SPECTRAL VELOCITY
AVERAGE SHEAR WAVE VELOCITY
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RESPONSE OF SOIL
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Filling materials
Sandy silt
Medium to stiff clayey
silt of low plasticity
30 m Input motion: 6.9 Magnitude earthquake
with epicentral distance of 34 km, PHA =
0.32 g
Surface: Amplified 7.788 times
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Peak Horizontal Acceleration (g)
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BKTPATAN
THAMEL
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Peak Spectral Acceleration (g)
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BKT
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PATAN
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Amplification factor
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Peak Spectral Velocity (cm/s)
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RESEARCH HORIZON
Development of Vs-N relationship for Kathmandu
valley
Assessment of signal attenuated at local site
Development of site specific design spectra using
‘ NONLIN’
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ACKNOWLEDGEMENTS
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Thank you for your kind presence !!!
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