lessons learnt from the recent off the pacific coast of tohoku earthquake in japan

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    Lessons Learnt from the Recent Off the

    International Platform for Reducing Earthquake Disasters (IPRED)

    26~28-07-2011 UNESCO-IPRED 4th Workshop, in Santiago, CHILE

    Japan

    Research Coordinator

    Building Research InstituteIncorporated Administrative Agency, Japan

    1

    The Mw 9.0 earthquake occurred off

    the Pacific coast of Tohoku, Japan at

    14:46 JST on 11th March 2011.

    This magnitude ranked fourth

    IntroductionIntroduction

    A

    40N

    Tohoku

    NAM PAC

    among the earthquakes in the world

    since 1900.

    The earthquake caused extremelydestructive tsunami.

    In addition to loss of lives and

    Mw 9.0

    B

    38N

    36N

    142E140E 146144E

    JT

    destruction of buildings, the tsunami

    induced nuclear serious accidents in

    Fukushima Daiichi Nuclear Power

    Plants, where the response activity is

    still in process.2

    0

    50

    100

    150Depth(km)

    -100 0 100 200 300

    Distance (km)

    A B

    Relocated aftershocks by

    Hurukawa (2011 EPS)

    http://www.terrapub.co.jp/journals/EPS

    /pdf/free/inpress/201105027.pdf

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    3

    1. Strong motion observations for building structures

    2. Field Surveys of damage to buildings

    1) Outline

    2) Damage to buildings caused by Seismic motion

    4) Damage to buildings caused by Fire

    3. Technical support to the Ministry of Land, Infrastructure,

    Transport and Tourism

    4. Information uploads

    5. Activit ies on going

    Many research activities and field survey were carried out jointly by

    National Institute for Land and Infrastructure Management (NILIM) and

    Building Research Institute (BRI).

    Ill introduce results obtained by staff members of NILIM and BRI.

    5

    1. Strong motion observations for building structures

    54 among 74 sites observed the mainshock134 135 136 137 138 139 140 141 142 143 144 14

    5 146

    44 44

    38 38

    39 39

    40 40

    41 41

    42 42

    43 43

    2011/03/11

    14:46(JST)THU, SND

    HCN2, HCNHRH

    AKT

    TRO

    NIG

    HKD

    HKUKGC

    HRO

    MYK

    13920' 13940' 14000' 14020' 140 40'

    ' 4 '

    3600' 3600'

    3620' 3620'

    ANX, BRI

    NIT

    TUS

    TKC

    YCYFNB

    EDG

    UTK,NMW,SMD

    ADC

    MSTTDSAKB

    KDI NKN

    SITA, SIT2

    6

    134 135 136 137 138 139 140 141 142 143 144 145 146

    34 34

    35 35

    36 36

    37 37

    0 100 200

    km

    h=24 km, M9.0

    NGN

    YMN

    SMZSMS

    NGY

    MTS

    OSK

    KSOMIZ

    IWK

    13920' 139 40' 14000' 140 20' 140 40'

    3520' 3520'

    0 50

    km

    CGC,CG2,CG3

    CHBTUF

    KWS

    http://smo.kenken.go.jp/

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    Strong ground motions with large

    seismic intensities138 139 140 141 142 143

    40

    Acceleration

    -3000

    0

    3000

    (cm/s2)

    N-S (peak: 2679 cm/s2)

    0

    3000

    (cm/s2)

    E-W(peak:- 1285 cm/s2)

    Pseudo Vel. Resp. Spectrum (h=5%)

    50

    100

    500

    locityResponse(cm/s)

    100

    )

    100

    1000

    1000

    0K-Net

    37

    38

    39

    -3000

    -3000

    0

    3000

    (cm/s2)

    0 20 40 60 80 100 120 140 160 180 200Time (sec)

    U-D (peak: 1886 cm/s2)

    2

    5

    10

    PseudoVe

    0.1 0.5 1 5 10Period (sec)

    0.1(cm) 1

    1010(cm/s/s

    N-SE-WU-D

    MYG004: K-NETTsukid ateAcceleration

    -3000

    0

    3000

    (cm/s2)

    N-S (peak: 1520 cm/s2)

    -3000

    0

    3000

    (cm/s2)

    E-W(peak: 987 cm/s2)

    -3000

    0

    3000

    (cm/s2)

    0 20 40 60 80 100 120 140 160 180 200Time (sec

    U-D (peak:- 299 cm/s2)

    Pseudo Vel. Resp. Spectrum (h=5%)

    2

    5

    10

    50

    100

    500

    PseudoVelocityResponse(cm/s)

    0.1 0.5 1 5 10Period (sec

    0.1(cm) 1

    10

    100

    10(cm/s/s)

    100

    1000

    1000

    0

    N-SE-WU-D

    K-NET Tsukidate(MYG004)

    K-NET Sendai(MYG013)

    K-NET Hitachi

    7

    138 139 140 141 142 143

    35

    36

    0 50 100

    km

    MYG013: K-NET SendaiAcceleration

    -3000

    0

    3000

    (cm/s2)

    N-S (peak:- 1599 cm/s2)

    -3000

    0

    3000

    (cm/s2)

    E-W(peak:- 1187 cm/s2)

    -3000

    0

    3000

    (cm/s2)

    0 20 40 60 80 100 120 140 160 180 200Time (sec)

    U-D (peak: 1159 cm/s2)

    Pseudo Vel. Resp. Spectrum (h=5%)

    2

    5

    10

    50

    100

    500

    PseudoVelocityResponse(cm/s)

    0.1 0.5 1 5 10Period (sec)

    0.1(cm) 1

    10

    100

    10(cm/s/s)

    100

    1000

    1000

    0

    N-SE-WU-D

    IBR003: K-NET Hitachi

    1 G or more at 20 sites. But less damage to buildings. Due to shorter predominant periods.

    Nine-story school building of

    Tohoku Univ., Sendai

    0

    1000

    c(gal)

    (a) Acc. in N192E

    01F(N192E)09F(N192E)

    1000

    Ac

    1000

    0

    1000

    Acc(gal)

    (b) Acc. in N282E

    40

    0

    40

    Disp(cm)

    (c) Rel.Disp. in N192E

    0

    40

    (cm)

    (d) Rel.Disp. in N282E

    01F(N282E)09F(N282E)

    8

    40

    Dis

    0.5

    1.0

    1.5

    2.0

    T(s)

    0 50 100 150 200

    Time (s)

    (e) Natural period

    N192E N282E

    Lessons:

    We could observe a damage

    process of the building. It leads to1) Application to health monitoring.

    2) Testing of non-linear response

    analysis method.Temporal change of national period of the building.

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    2. Field Surveys of damage to build ings

    1) Outline2) Damage to buildings caused by Seismic motion

    Timber Structure Reinforced Concrete Structure Steel Structure, Non-Structural Elements Housing-Site Ground, Foundations

    3) Damage to buildings caused by Tsunami) Damage to buildings caused by Tsunami4) Damage to buildings caused by Fire

    11

    1) Outline

    Organizing field surveyteams to learn lessonsfrom structural damage

    MiyakoCityOtsuchiTownYamadaTown

    OfunatoCityKamaishiCity

    Rikuzentakata CityKesennumaCity

    MinamisanrikuTownIshinomakiCity

    Kitakami CityHiraizumiTown

    TonoCity

    KuriharaCity

    Iwate

    Miyagifrom structural damagestate, BRI and NILIM aredispatching more than140experts to the surveyareas since March 12.

    OnagawaTownHigashimatsushimaCityMatsushimaTown

    ShiogamaCityShichigahamaTownTagajoCitySendaiCityNatoriCityWatariTownIwanumaCityYamamotoTown

    ShiroishiCityNihonmatsuCityFukushimaCityMiharuTown

    KoriyamaCityNasuTownYaitaCity

    Fukushima

    12SurveyAreasinCitiesandTownsNames

    SukagawaCityShirakawaCity

    Hitachiota CityHitachiCityNakaCityHitachinakaCity

    MitoCityOaraiTownOmitamaCityHokotaCity

    rosa o ownKasamaCity

    ChikuseiCityShimotsumaCity

    KogaCityBandoCity

    JosoCityTsuchiuraCityRyugasakiCity

    UrayasuCity

    KashimaCityItakoCity

    KamisuCityInashikiCitySakaeTown

    BRI / NILIM

    Ibaraki

    Tochigi

    Chiba

    0 50km

    Tokyo

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    Damage to RC Structure

    15

    1st story of 3 storied RC buildingwas collapsed. Front side is

    frame structure and back side is

    frame with wall structure.

    Shear failure in columnson 1st story of 4 storied RC

    building which shows 180

    degree hooks of main bars.

    Damage to Steel Structure and Non-Structural Elements

    16

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    Damage to Housing-Site Groundand Foundations

    17

    Damage to buildings caused by seismic motion

    Damage to buildings is not so severe whereas the seismic

    intensities were high and the disaster areas were extended to

    extremely large.

    Timber StructureTypical seismic damage was observed.

    RC StructureSignificant difference appears between before and

    after the new seismic design code (1981). Typical seismic damage

    was observed.

    Steel StructureDamage to vertical / horizontal braces and joints

    was observed.

    Non-structural ElementsThe fall of exterior walls sus ended

    ceilings in large-scale spaces, and interior materials were observed.

    Damage occurred in some grounds of developed residential areas

    and sloping areas.

    The severe liquefaction damage occurred in very wide areas.

    18

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    3) Damage to bui ldings caused by Tsunami BRI and NILIM have jointly carried out

    damage surveys three times since March 11th

    to understand the general status of damageto buildin sIwate .

    Team #1 30 March 2 April

    Rikuzentakata (IWATE) , Kesennuma, Minami-sanriku,

    Onagawa, Ishinomaki, Natori (MIYAGI)

    Team #2 6 -9 April

    Yamada, Ohtsuchi, Kamaishi, Ohfunato, Rikuzentakata (IWATE),

    Onagawa (MIYAGII) etc.

    Team #3 6 8 April

    Miyagi

    19

    , , , .

    Data related to water depth and dimension indamaged buildings were also extensivelycollected. They are supposed to be muchinformative for the estimation of the effect oftsunami loads and also for the verification ofthe current design guidelines.

    Fukushima

    Survey areas

    Damage to RC Structure

    Colla se of 1st stor of 2 Fallin over of 4 storied RC

    20

    storied RC frame building with

    concrete brick wall. The 2nd

    story was supported by 4 RC

    columns.

    frame building with shear wall.

    This building was flowed 70

    meters.

    Photo shows the undersurface

    and a faade.

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    Damage to RC StructureBuildings swept-away and fallen-over

    4-story frame with shear wall structure

    - ,

    Few Openings

    Swept-away (70 m, no traces of dragged)

    Fallen-over

    Distance from the coast~200 m

    Depth of inundation~15 m 21

    Damage to RC StructureBuildings swept-away and fallen-over

    22

    2-story frame structure

    (refrigerators)

    Few openings

    Swept-away and fallen-over

    Distance from the coast~200 m

    Depth of inundationOver 6.5 m

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    Damage to RC Structure

    3 storied RC factory building4 storied RC frame building

    Out of lane colla se of

    23

    .

    Photo shows the footing

    basement under columns.

    exterior wall with frame andwithout inside floor.

    The right side of photo shows

    no collapse of wall with floor.

    Damage to Steel Structure

    24

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    Damage to Timber Structure

    25

    building z

    Review for Tsunami Evacuation Bui lding

    Evaluation Method of Tsunami

    Evacuation Building

    The Cabinet Office : Proposal equation of

    Guideline for tsunami evacuation

    3h

    3gh

    zq

    pressure is applied using the threefolddepth of design wave depth.

    Design wave depth: h

    Design wave pressure

    Based on the surveyed results, the validity of the above-mentioned

    Tsunami Load (Tsunami Wave Pressure) is under reviewing.

    26

    z

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    2011 Miyako, Iwate (IISEE/BRI)

    Break water in

    Miyako

    2011 Miyako, Iwate (IISEE/BRI)

    May 14, 2010

    April 2011

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    World largest

    break water

    in Kamaishi

    1,660 m long & 63 m height

    1/3 collapsed, but

    Tsunami height was reduced 40 %.

    Arrival time delayed 6 min.

    (Kamaishi Port Office)

    2011 Miyako, Iwate (IISEE/BRI)

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    2011 Miyako, Iwate (IISEE/BRI)

    2011 Miyako, Iwate (IISEE/BRI)

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    2011 Ootsuchi, Iwate (IISEE/BRI)

    2011 Onagawa, Miyagi (IISEE/BRI)

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    2011 Onagawa, Miyagi (IISEE/BRI)

    2011 Onagawa, Miyagi (IISEE/BRI)

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    2011 Onagawa, Miyagi (IISEE/BRI)

    2011 Onagawa, Miyagi (IISEE/BRI)

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    2011 Onagawa, Miyagi (IISEE/BRI)

    2011 Onagawa, Miyagi (IISEE/BRI)

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    2011 Sendai, Miyagi (IISEE/BRI)

    2011 Sendai, Miyagi (IISEE/BRI)

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    2011 Sendai, Miyagi (IISEE/BRI)

    2011 Sendai, Miyagi (IISEE/BRI)

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    2011 Sendai, Miyagi (IISEE/BRI)

    2011 Iwaki, Fukushima (IISEE/BRI)

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    2011 Iwaki, Fukushima (IISEE/BRI)

    2011 Iwaki, Fukushima (IISEE/BRI)

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    2011 Iwaki, Fukushima (IISEE/BRI)

    2011 Iwaki, Fukushima (IISEE/BRI)

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    3. Technical support to the Ministry of Land,

    Infrastructure, Transport and Tourism (MILIT)

    Collaborative Research with private companies in thedevelopment and promotion project of building standards.1: Consideration of contributing to the development of building

    standards in tsunami hazard areas

    2: Consideration of contributing to the development of non-structural elements standard based on earthquake damage

    3: Consideration of the effect of long-period seismic motion onsuper high-rise buildings

    Building Structural Standard Committee (NILIM)

    57

    Cooperate in research surveys and investigations of this committeeappointed to consider the draft of building structural standard

    Committee of Technical Countermeasure againstLiquefaction (MILIT)

    Participate as a member in this committee appointed to considertechnical issues common in each infrastructure

    4. Information uploads

    Established the special website to provide official information

    http://iisee.kenken.go.jp/special2/

    to o u. tm

    58

    http://www.kenken.go.jp/japanese/con

    tents/topics/20110311

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    Produced Quick Report of the

    Field Survey and Research on

    The 2011 Off the Pacific coast

    of Tohoku Earthquake jointly

    with NILIM and announced on

    the special web site on May 13,

    2011.

    * English version will be released

    on the end of August.

    59

    5. Activit ies on going

    Continuation and expansion of the field survey and

    research works, and quick release and dissemination of

    u .

    Active participation and technical support to activities bythe national government.

    Close coo eration with concerned or anizations such as

    Architectural Institute of Japan (AIJ).

    60