effects of deep intraplate earthquakes in subduction...
TRANSCRIPT
Effects of deep intraplate
earthquakes in subduction
zones
Dr. Freddy E. Pina, P.Eng.PBRV Consulting Ltd.
The University of British Columbia
August 2013, Vancouver, BC
Subduction Zones
GEIYO 2001 – Mw 6.7
• Deep quake - 50km
• 3700 Buildings damaged
• 2 casualties
NISQUALLY 2001 – Mw 6.8
• Deep quake - 52km
• $1 billion losses
• 1 casualty + 400 injured
El Salvador 2001 – Mw 7.7
• Deep quake – 60 km
• $1.2 billion losses
• 800 casualty (landslide)
Punitaqui 1997 – Mw 7.1
• Deep quake – 100 km
• 8 deaths
• 60000 homeless
Estimating impact of deep quakes
• Part I: Santiago, Chile
– Preliminary risk estimates vs Subduction
quakes
– Study per municipalities
• Part II: Vancouver, BC
– Risk estimates
– Impact in the BC public school seismic
assessment/retrofit program
Chile Subduction
Location of selected earthquakes
SantiagoCoast Mountain
Epicenter Date MagnitudeNo.
Stations
Distance
Range
(km)
Elastic Spectra - Santiago - Site Class C
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
0.01 0.10 1.00 10.00
Period (s)
Sa
(g
)
Subduction - Median
Subduction - 84th %ile
Subduccion - Max
Deep - Median
Deep - 84th %ile
Deep - Max
Code
Elastic Spectra - Santiago - Site Class C
0.0
0.2
0.4
0.6
0.8
1.0
1.2
0.01 0.10 1.00 10.00
Period (s)
Sa
(g
)
Subduction - Median
Subduction - 84th %ile
Deep - Median
Deep - 84th %ile
Code
Comparison
• In terms of earthquake shaking:
– Subduction dominates hazard values for most
periods
– Large deep quake spectral accelerations at
periods shorter than 0.5sec
• However, we need to see responses in
terms of structural parameters…
Santiago, Chile
• 34 districts (municipalities)
• 5.4 million people
• 1.45 million houses (urban areas)
1- to 2-
storey
houses
4- to 15-
storey
buildings
Main material/systems
Confined Masonry
Wood housesRC buildings
Structural system classification
Group Structural No of % in Estimated Estimated R factor
Name System storeys Santiago Period - sec Ductility factor (Miranda 1993)
G1 - MASONRY 2S Confined Masonry 2 49 0.2 2 1.8
G2 - MASONRY 4S Confined Masonry 4 8 0.4 2 2.0
G3 - CONCRETE 2S Reinforced Concrete Walls 2 8 0.2 2 1.8
G4 - CONCRETE 5S Reinforced Concrete Walls 5 5 0.5 3 2.9
G5 - CONCRETE 10S Reinforced Concrete Walls 10 4 1.0 5 4.8
G6 - CONCRETE 15S Reinforced Concrete Walls 15 2 1.5 5 5.0
G7 - CONCRETE 20S Reinforced Concrete Walls 20 1 2.0 6 6.0
G8 - CONCRETE 30S Reinforced Concrete Walls 30 1 3.0 6 6.0
G9 - CONCRETE 10S Wood Shear Walls 2 10 0.2 5 2.9
Ductility = 2.0
Ductility = 6.0
Risk = Probability of Code values
being exceeded
G1 -
MA
SO
NR
Y 2
S
G2 -
MA
SO
NR
Y 4
S
G3 -
CO
NC
RE
TE
2S
G4 -
CO
NC
RE
TE
5S
G5 -
CO
NC
RE
TE
10S
G6 -
CO
NC
RE
TE
15S
G7 -
CO
NC
RE
TE
20S
G8 -
CO
NC
RE
TE
30S
G9 -
WO
OD
2S
0%
5%
10%
15%
20%
25%
30%
DEEP
SUBDUCTION
Main comments
• Current code does not address the effect of deep earthquakes, specially for short period structures, e.g. confined masonry houses
• Although deep quake hazard values are lower than that for subduction quakes, the effect of deep quake motions to a wide range of structures is likely to be similar
What’s next…
• Define design spectral values or recommendations to address deep quakes in Chile
• Next Part using SRG methodology
– Vancouver
– Victoria
– Interior BC
– Santiago
• Define ground motion records for risk calculations
Cascadia Subduction
& Vancouver – H Model ?
& Vancouver – H Model ?
Elastic Spectra - Santiago - Site Class C
0.0
0.2
0.4
0.6
0.8
1.0
1.2
0.01 0.10 1.00 10.00
Period (s)
Sa
(g
)
Subduction - Median
Subduction - 84th %ile
Deep - Median
Deep - 84th %ile
Code
Deep - H Model - Vancouver
Lower values for short periods
Elastic Spectra - Santiago - Site Class C
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
0.01 0.10 1.00 10.00
Period (s)
Sa
(g
)
Deep - Median
Deep - 84th %ile
Deep - Max
Code
Deep - Model H - Vancouver
Lager values for long periods
Elastic Spectra - Santiago - Site Class C
0.0
0.2
0.4
0.6
0.8
1.0
0.10 1.00 10.00
Period (s)
Sa
(g
)
Deep - Median
Deep - 84th %ile
Deep - Max
Code
Deep - Model H - Vancouver
Recommended New Suites of Seed
Time Histories for SRG Database
• 11 Pairs from Crustal Earthquakes for Most Prototypes– Expected period longer than 1 sec
– Expected period between 0.5 and 1 sec with ductility larger than or equal to 2
– Scaling based on PSV* average
• 11 Pairs from Subcrustal Earthquakes for Other Prototypes– Expected period shorter than 0.5 sec
– Expected period between 0.5 and 1 sec with ductility smaller than 2
– Scaling based on Max Spectral Acceleration
Recommended New Suites of Seed
Time Histories for SRG Database
• 3 x 11 Pairs from Subduction Earthquakes for
All Prototypes
– Divide Province in 3 Zones
• Zone 1: Estimated Rupture Area + 25km
• Zone 2: 25km from Rupture Area + 100km
• Zone 3: 100km from Rupture Area
Thanks