chile presentation hanping hong
TRANSCRIPT
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Some Observations from Recent
Dept. of Civil & Environmental Eng.
University of Western Ontario
, ,
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e ven : e ear qua e
Date: February 27, 2010=
Epicenter: 35.909oS 72.733oW at a depthof about 35 km.
Location: Offshore Maule, in a subductionzone in which the Nazca late asseseastward and downward beneath theSouth American plate, with a rate ofconvergence o a out 7 mm year.
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Seismicity
http://www.nytimes.com/interactive/20
10/02/27/world/americas/0227-chile-
quake-map.html
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Seismicity
http://neic.usgs.gov/neis/eq_depot/2010/eq
_100227_tfan/neic_tfan_c.html
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Possible available ground motion records
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n orma on romInformation based on preliminary report by Boroschek et al.
(2010) using records from RENADIC.
Peak vertical
ground
acceleration
Peak hor izontal
ground
accelerationStation
Peak vertical
ground
acceleration
Peak hor izontal
ground
accelerationStation
Estacion Metro Mirador
0.140.17
Universidad de Chile, Dept. Ing.
Civil (interior Edificio) Sandiago
Estacion Metro Mirador
0.140.17
Universidad de Chile, Dept. Ing.
Civil (interior Edificio) Sandiago
0.130.27Hosp. Sotero de Rio RM
0.280.30Hosp. Tisner RM
0.240.56CRS Maipu RM
..
0.130.27Hosp. Sotero de Rio RM
0.280.30Hosp. Tisner RM
0.240.56CRS Maipu RM
..
0.260.35Vina del Mar (Marga Marga)
0.050.14Hosp. Valdiv ia
0.200.47Hosp. Curico
0.260.35Vina del Mar (Marga Marga)
0.050.14Hosp. Valdiv ia
0.200.47Hosp. Curico
.. ..
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Ground motion records at Estacion Metro Mirador Santiago.
Boroschek et al. (2010). Digital records is sti ll not widely available.
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Response Spectra for Estacion Metro Mirador Santiago (Boroschek et al. 2010).
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, ,
although the terminals are closed and a temporary tent and laptops are used by
off icers (March 8, 2010). Certainly, there is business interrupt ion costassociated with it.
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A building in Concepcion
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A building in Concepcion: Interstory collapse and will be demolished.
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Examples of buildings that survived this earthquake
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Partial damage. Possible consequences
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A damaged building in Chillan
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Twin build ings: the damage in one
is more signi ficant then the other
Chillan)
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Adobe constructions
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A street view in Talco
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Brid esThe Llacoln Bridge in
Concepcin was constructed in
.
traffic and pedestrian access to
downtown Concepcin)
The Llacoln bridge in Concepcin (Report of the NSF Sponsored GEER
Association Team, Edited by J. Bray and D. Frost
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Deck unseating at Llacoln bridge
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This is a old bridge and it was not in service for several years.
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Juan Pablo II bridge connects the cities of Concepcin and San Pedro de laPaz. It opened to the public in 1974. The bridge consists of 70 spans (L = 33m, W = 21.9 m) each one composed of 7 reinforced concrete girders and aconcrete slab. The se ments sit on reinforced concrete bents with drilled ierSupports. (Report of the NSF Sponsored GEER Association Team, Edited by J.Bray and D. Frost
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A damaged highway bridge
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A damaged highway overpass
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Effect of tsunami
in Talcahuano
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In
Pelluhue
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Some observed non-en ineered re air
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Unreinforced adobe houses should not be used orstrengthened in the seismic region to minimizethe seismic vulnerability.
an new s ruc ures can e vu nera e ur ngan earthquake
Emer enc education and ractice for naturaldisasters contributes to the safety of locals, butis not effective for visitors or tourists.
e rus o non-eng neere repa r re roshould be highly discouraged, even though thereis a need to restore normal life.