Brief review of building damage by the 2011 Tohoku Japan earthquake and following coping activities

Similar documents
SAFETY EVALUATION OF SEISMICALLY ISOLATED HOUSES WITH DISPLACEMENT RESTRAINT DEVICES UNDER SEVERE EARTHQUAKE MOTIONS

Field Investigation and Dynamic Analysis of Damaged Structure on Pile Foundation during the 2011 off the Pacific Coast of Tohoku Earthquake

Response characteristics of R/C buildings considering impulsive force of tsunami drifting objects

New Seismic Activity Model of Large Earthquakes along Nankai Trough for Probabilistic Seismic Hazard Maps

Source modeling of hypothetical Tokai-Tonankai-Nankai, Japan, earthquake and strong ground motion simulation using the empirical Green s functions

REPORT ON THE TOHOKU AREA PASIFIC OFFSHORE EARTHQUAKE

RELATIONSHIP OF SEISMIC RESPONSES AND STRENGTH INDEXES OF GROUND MOTIONS FOR NPP STRUCTURES

RELATIONSHIP BETWEEN AGE OF GROUND AND LIQUEFACTION OCCURRENCE IN THE 2011 GREAT EAST JAPAN EARTHQUAKE

Structures Group Report

Seismic Activity and Crustal Deformation after the 2011 Off the Pacific Coast of Tohoku Earthquake

CHARACTERISTICS OF STRONG GROUND MOTION FROM THE 2011 GIGANTIC TOHOKU, JAPAN EARTHQUAKE

Simulated Earthquake Ground Motion for Structural Design"

Earthquakes and Earth s Interior

Special edition paper


- Information before strong ground motion -

Deterministic and Non-deterministic Behavior of Earthquakes and Hazard Mitigation Strategy

Prevention Tsunami wall 10m high (breached by the tsunami due to land level falling by 3m)

Study of the liquefaction phenomenon due to an earthquake: case study of Urayasu city

Lessons Learned from Past Tsunamis Warning and Emergency Response

Preliminary report of the 2011 off the Pacific coast of Tohoku Earthquake *

SIMPLIFIED METHOD IN EVALUATING LIQUEFACTION OCCURRENCE AGAINST HUGE OCEAN TRENCH EARTHQUAKE

EFFECTIVE STRESS ANALYSES OF TWO SITES WITH DIFFERENT EXTENT OF LIQUEFACTION DURING EAST JAPAN EARTHQUAKE

Downtown Anchorage Seismic Risk Assessment & Land Use Regulations to Mitigate Seismic Risk

PRELIMINARY STUDY OF GROUND MOTION CHARACTERISTICS IN FURUKAWA DISTRICT, JAPAN, BASED ON VERY DENSE SEISMIC-ARRAY-OBSERVATION

Title. Author(s)DONG, Q.; OKAZAKI, T.; MIDORIKAWA, M.; RYAN, K.; SAT. Issue Date Doc URL. Type. Note. File Information BEARINGS

S. Toda, S. Okada, D. Ishimura, and Y. Niwa International Research Institute of Disaster Science, Tohoku University, Japan

Special Contribution Measures for Earthquake and Tsunami Resilience Enhancement of Industrial Parks in Bay Areas

Section Forces Within Earth. 8 th Grade Earth & Space Science - Class Notes

Risk-based land use and spatial planning

Collapse modes of structures under strong motions of earthquake

Earthquakes.

Sendai Earthquake NE Japan March 11, Some explanatory slides Bob Stern, Dave Scholl, others updated March

Application of Capacity Spectrum Method to timber houses considering shear deformation of horizontal frames

Wainui Beach Management Strategy (WBMS) Summary of Existing Documents. GNS Tsunami Reports

Ömer AYDAN. Ismail FEBRIN. Fumihiko IMAMURA KOGAMI (Tsunami Alert Community-NPO)

A STUDY ON DAMAGE TO STEEL PIPE PILE FOUNDATION ON RECLAIMED LAND DURING HYOGO-KEN-NANBU EARTHQUAKE

Guidelines for Site-Specific Seismic Hazard Reports for Essential and Hazardous Facilities and Major and Special-Occupancy Structures in Oregon

Shake Table Tests of Reinforced Concrete Bridge Columns Under Long Duration Ground Motions

REPORT TO THE PLANNING, TRANSPORTATION AND PROTECTIVE SERVICES COMMITTEE MEETING OF JUNE 26, 2013

Chapter 6 Seismic Design of Bridges. Kazuhiko Kawashima Tokyo Institute of Technology

Long-period Ground Motion Characteristics of the Osaka Sedimentary Basin during the 2011 Great Tohoku Earthquake

Three Fs of earthquakes: forces, faults, and friction. Slow accumulation and rapid release of elastic energy.

Tsukuba, Japan International Institute of Seismology and Earthquake Engineering Building Research Institute STUDY TRIP TO ITAKO CITY

2.3 Notes: Earthquake Damage Can Be Reduced

I. Locations of Earthquakes. Announcements. Earthquakes Ch. 5. video Northridge, California earthquake, lecture on Chapter 5 Earthquakes!

A Study on the Risk Assessment of Emergency Supplies. Transportation Routes Considering Scenario Earthquakes

SEISMIC PERFORMANCE OF URBAN, RECLAIMED AND PORT AREAS -FULL SCALE EXPERIMENT USING BLAST TECHNIQUE. Takahiro SUGANO 1) and Eiji KOHAMA 2)

Forces in Earth s Crust

Residual Deformation Analyses to Demonstrate the Effect of Thin Steel Sheet Piles on Liquefaction-Induced Penetration Settlement of Wooden Houses

Study on acceleration response spectra for seismic design based on observed records in Hokkaido, JAPAN

Crustal deformation by the Southeast-off Kii Peninsula Earthquake

Micro Seismic Hazard Analysis

THEORETICAL EVALUATION OF EFFECTS OF SEA ON SEISMIC GROUND MOTION

On The Ultimate Strength of RC Shear Wall under Multi-Axes Seismic Loading Condition

What is an Earthquake?

VERIFICATION TEST AND EARTHQUAKE RESPONSE OBSERVATION OF A BASE ISOLATED BUILDING WITH ECCENTRIC ROLLER BEARINGS

Preliminary Analysis for Characteristics of Strong Ground Motion from Gigantic Earthquakes

Section 19.1: Forces Within Earth Section 19.2: Seismic Waves and Earth s Interior Section 19.3: Measuring and Locating.

PILE FOUNDATION RESPONSE DUE TO SOIL LATERAL SPREADING DURING HYOGO-KEN NANBU EARTHQUAKE

Real time Monitoring System for Earthquakes and Tsunamis (DONET)

New model for Shear Failure of R/C Beam-Column Joints. Hitoshi Shiohara

APPLICATON OF SEAMLESS SIMULATION OF SEISMIC RESPONSE ANALYSIS AND HIGH RESOLUTION TSUNAMI SIMULATION TO COASTAL AREA OF SENDAI

Depth-dependent slip regime on the plate interface revealed from slow earthquake activities in the Nankai subduction zone

Sabah Shawkat Cabinet of Structural Engineering Walls carrying vertical loads should be designed as columns. Basically walls are designed in

HORIZONTAL LOAD DISTRIBUTION WITHIN PILE GROUP IN LIQUEFIED GROUND

SHAKING TABLE TESTS ON SEISMIC RESPONSE REDUCTION EFFECTS OF ROCKING BUILDING STRUCTURAL SYSTEMS

STRONG GROUND MOTION PREDICTION FOR HUGE SUBDUCTION EARTHQUAKES USING A CHARACTERIZED SOURCE MODEL AND SEVERAL SIMULATION TECHNIQUES

Outline of Guideline for Development and Utilization of Tsunami Disaster Management Map

STRONG MOTION RECORDS FROM THE 2011 OFF THE PACIFIC COAST OF TOHOKU EARTHQUAKE

Source Characteristics of Large Outer Rise Earthquakes in the Pacific Plate

NUMERICAL ANALYSIS OF DAMAGE OF RIVER EMBANKMENT ON SOFT SOIL DEPOSIT DUE TO EARTHQUAKES WITH LONG DURATION TIME

Preliminary Examination in Dynamics

Real Time Monitoring System for Megathrust Earthquakes and Tsunamis - Cabled Network System and Buoy System in Japan -

Centrifuge Shaking Table Tests and FEM Analyses of RC Pile Foundation and Underground Structure

Evaluating the effects of near-field earthquakes on the behavior of moment resisting frames

PROBABILISTIC SEISMIC HAZARD MAPS AT GROUND SURFACE IN JAPAN BASED ON SITE EFFECTS ESTIMATED FROM OBSERVED STRONG-MOTION RECORDS

A STUDY AND DEVELOPMENT OF SEMI-ACTIVE CONTROL METHOD BY MAGNETORHEOLOGICAL FLUID DAMPER IN BASE ISOLATED STRUCTURES

at IHO IRCC7 Mexico City, Mexico, June 2015

RESPONSE ANALYSIS STUDY OF A BASE-ISOLATED BUILDING BASED

GROUND MOTION SPECTRAL INTENSITY PREDICTION WITH STOCHASTIC GREEN S FUNCTION METHOD FOR HYPOTHETICAL GREAT EARTHQUAKES ALONG THE NANKAI TROUGH, JAPAN

STRESS IN THE SYSTEM? INSIGHTS INTO MODELLING IN THE WAKE OF TOHOKU

Earthquakes and Tsunamis

Earthquake Hazards. Tsunami

An entire branch of Earth science, called, is devoted to the study of earthquakes.

Design of a Multi-Storied RC Building

Magnitude 6.5 OFFSHORE NORTHERN CALIFORNIA

SEISMIC PERFORMANCE EVALUATION METHOD FOR A BUILDING WITH CENTER CORE REINFORCED CONCRETE WALLS AND EXTERIOR STEEL FLAME

Earthquake hazards. Aims 1. To know how hazards are classified 2. To be able to explain how the hazards occur 3. To be able to rank order hazards

Fujinuma Dam Performance during 2011 Tohoku Earthquake, Japan and Failure Mechanism by FEM

The impact of the 2011 off the Pacific coast of Tohoku Earthquake on Tsukuba 32-m station

Interpretive Map Series 24

KNOWLEDGE NOTE 5-1. Risk Assessment and Hazard Mapping. CLUSTER 5: Hazard and Risk Information and Decision Making. Public Disclosure Authorized

Tohoku-oki event: Tectonic setting

EARTHQUAKE OBSERVATION OF A LOW-RISE BUILDING

RESIDUAL STORY-DRIFT OF WEAK-BEAM PORTAL FRAME WITH SLIP-TYPE RESTORING FORCE CHARACTERISTICS OF COLUMN-BASE SUBJECTED TO GROUND MOTION

Name Date Class. radiate in all directions, carrying some of the. of plate boundaries have different usual patterns of.

EUROCODE EN SEISMIC DESIGN OF BRIDGES

Geotechnical Extreme Events Reconnaissance Report:

CHARACTERISTICS OF SOURCE SPECTRA OF SMALL AND LARGE INTERMEDIATE DEPTH EARTHQUAKES AROUND HOKKAIDO, JAPAN

Transcription:

1 Brief review of building damage by the 211 Tohoku Japan earthquake and following coping activities Isao Nishiyama* (BRI), Izuru Okawa (BRI), Hiroshi Fukuyama (BRI) and Yasuo Okuda (NILIM) BRI : Building Research Institute NILIM : National Institute for Land & Infrastructure Management 14 th U.S.-Japan Workshop on Improvement of Structural Design and Construction Practices December 3-5, 212, Makena Beach & Golf Resort

1. Introduction 2

JMA Seismic Intensity & Hypocentral Region 3 Tohoku earthquake Mw=9. (14:46 JST on March 11, 211) 45km (NS) x 15km (EW)

4 Building and Residential Land Damage by Earthquake Motion and Tsunami BRI and NILIM sent 43 teams for field survey and the following reports are available as of December 2, 212 http://www.kenken.go.jp/japanese/cont ents/publications/data/132/index.html http://www.kenken.go.jp/japanese/cont ents/publications/data/135/index.html http://www.kenken.go.jp/japanese/cont ents/topics/211311/311report.html http://www.kenken.go.jp/japanese/cont ents/publications/data/138/index.html http://www.kenken.go.jp/english/conte nts/topics/211311/311summaryrepo rt.html

2. Recorded Ground and Building Motions 5

142 141 14 4' 14 2' 14 4' 14 2' 142 141 6 BRI Strong Motion Network 146 145 144 143 44 14 139 138 137 136 135 134 44 139 4' 139 2' 43 43 42 42 41 41 4 4 AKT 39 39 TRO 38 NIG THU, SND 38 37 37 NGN 36 36 MIZ IJMA KSO NGY 35 OSK, SKS YMN SMZ 35 SMS 34 MTS 7 6 5 4 3 2 1 ISK 34 146 145 144 143 14 HRH HKD HKU IWK HCN2, HCN TAMA2, MIYA2 MYK HRO KGC 211/3/11 14:46(JST) h=24 km, M9. km 139 4' 139 2' 1 2 14 ' 36 2' 36 2' 36 ' 36 ' UTK, NMW, SMD 35 4' 35 4' KDI NKN YYG CGC, CG2, CG3, NDLG, NDLM, NDLA YKH KWS NIT SITA, SIT2 TDS AKB TUF ADC EDG TKD TUS MST ICK MTK 35 2' 35 2' 14 ' FNB ANX, BRI, NCTD TKC YCY CHB km IJMA 5 7 6 5 4 3 2 1 139 138 137 136 135 134 In 1957, BRI started strong motion network.

Damaged Building in Sendai city Acc (cm/s 2 ) 1 1 1 Acc (cm/s 2 ) 1 4 Disp (cm) Disp (cm) T(s) 4 4 4 2. 1.5 1..5 (a) Acc. in Trans. Dir. (b) Acc. in Long. Dir. (c) Bldg. Disp. in Trans. Dir. (d) Bldg. Disp. in Long. Dir. (e) Transition of natural periods 7 5 1 15 2 Time (s) Trans 9F(Trans.) 1F(Trans.) 9F(Long.) 1F(Long.) Flexural failure of multi-story shear walls which can absorb large earthquake energy was observed. Though the building could secure human lives by preventing its collapse as demand of seismic codes, buckling and/or rupture of steel bars and steel plates in the columns and compressive crashing of concrete were observed. Finally, the building was demolished. Long.

8 Damaged Building in Sendai city (cont.) 1978 211 (cm/s 2 ) (cm/s 2 ) (cm/s 2 ) (cm/s 2 ) (cm/s 2 ) (cm/s 2 ) (cm/s 2 ) (cm/s 2 ) 1-1 1-1 1-1 1 22-1F (peak: 258 cm/s 2 ) 292-1F (peak:- 23 cm/s 2 ) 22-9F (peak: 14 cm/s 2 ) 292-9F (peak:- 529 cm/s 2 ) -1 2 4 6 8 1 12 14 16 18 2 Time (s) 1 192-1F (peak:- 333 cm/s 2 ) -1 1-1 1-1 1-1 282-1F (peak: 33 cm/s 2 ) 192-9F (peak: 98 cm/s 2 282-9F (peak: 728 cm/s 2 ) 2 4 6 8 1 12 14 16 18 2 Time (s) 1F(NS) 258 cm/s 2 1F(EW) 23 cm/s 2 9F(NS) 14 cm/s 2 9F(EW) 529 cm/s 2 1F(NS) 333 cm/s 2 1F(EW) 33 cm/s 2 9F(NS) 98 cm/s 2 9F(EW) 728 cm/s 2

52+3 story building in Osaka city 9-2 Disp. (cm)2-2 Disp. (cm)2-2 Disp. (cm)2-2 Disp. (cm)2-2 Disp. (cm)2-2 Disp. (cm)2 Displacement 1F SW-NE (peak:- 9.1 cm) 1F NW-SE (peak: 7.8 cm) 52F SW-NE (peak: 137.1 cm) 52F NW-SE (peak:- 83.7 cm) 52F-1F SW-NE (peak:- 138.2 cm) 52F-1F NW-SE (peak: 84.8 cm) 1 2 3 4 5 6 7 Time (s) Pseudo Vel. Resp.Spectrum (h=5%) 1 The large responses lasted at least 1 minutes in the building in Osaka, 77km from the epicenter. A 137cm maximum displacement occurred on the top floor. Many non-structural interior members such as ceilings, walls, fire doors, sprinklers, etc. were damaged, and even confinements of passengers in elevators occurred. Pseudo Velocity Response (cm/s) 5 1 5 1.5.1(cm) 1.1.5 1 5 1 Period (sec).1 1 1 1 1(cm/s/s) 1 SW-NE NW-SE

3. Building and Residential Land Damage 1

Field surveyed area by BRI and NILIM teams 11

Earthquake Motion Damage 12 Courtesy to the Japan MLIT

Earthquake Motion Damage (cont.) 13

Tsunami Damage 14

4. Coping Activities on Selected Issues 15

System to Revise Building Structural Codes 16 NILIM Building Structural Code Committee proposal MLIT Building Structural Code WG Long-duration longperiod earthquake ground motions TG Ceiling design method, etc. Private BRI R & D by self-budget technical advice On Building Structural Codes, * Proposal * Public comments * Technical information

1. Digital data by BRI strong motion network 2. Long-duration and long-period ground motion, structural performance under multiple cycles of loadings 3. Higher level of PBD, functional after earthquake 4. Fall down of ceilings in spatial structures and escalators in shopping centers 5. Fractured lead damper in seismically isolated buildings 6. Inclination due to liquefaction in residential houses 7. Evaluation of tsunami force 8. etc. 17

Long-duration and long-period ground motion prediction method based on observation at about 16 stations ORIGINAL EVALUATION MODEL 18 MLIT PROPOSAL FOR DESIGN MOTION CALL FOR PUBLIC COMMENTS, 21 211.3.11 Tohoku EQ. Revision of the model Philippine Sea plate Pacific plate Long-duration and long-period motion properties Spectral amplitudes from large earthquakes Duration of motions with each frequency band earthquake magnitude distance site specific coefficients (additional factors) Epicenters + Paths Earthquakes used in the analyses Revised evaluation method

36 36 19 Long-duration and long-period ground motion prediction method based on observation at about 16 stations (cont.) Long-duration and long-period motions were evaluated for major urban areas with two-, three- connected earthquakes, by HERP, CAO, AIJ, etc. MLIT is going to propose a design long-duration and long-period motions and is funding project for the purpose. HERP Nankai-trough three-connected earthquake model with revised model for major areas Nankai 32 km 32 1 2 132 136 14 CAO Mw9 model Osaka Nagoya Tokyo

Structural performance against long-duration and long-period ground motions (full-scale) 2 These large-size experiments are carried out under the research cooperation between the BRI and the institutions headed by Obayashi, Kajima and Taisei Co.

Fall down of ceilings in spatial structures After Geiyo earthquake (21), a technical advice was issued to recommend putting diagonal braces on ceiling rods, and keep clearance around suspended ceiling. (see left figure) Construction companies reported nearly 2, cases of fall down of ceilings during Tohoku earthquake. Examples with/without injury are compared. (see right figure) 21 Frequently observed damage by earthquake Recommended method in an MLIT technical advice Mass and height of ceiling damaged by earthquake

22 Fall down of ceilings in spatial structures (cont.) (Tentative) Allowable Stress Design for probable earthquake + safety margin Scope of regulation Ceiling height > 6m Ceiling area > 2m 2 Unit weight of ceiling > 2kg/m 2 Safety margin Vertical strength Clearance around ceiling

23 Fall down of escalators in shopping centers (Tentative) Requirement from H/1 (current) to H/4 (Tentative) Exceptional relaxation to H/1 in case of fall prevention device Roller overlapped Escalator truss Fixed H H/1 Escalator truss Floor Girder Connector Joint cover Fall prevention

24 Liquefaction Liquefaction evaluation was made by F L - method at 112 sites in Kanto area, the results were compared with observations. Liquefied sites ( ) are all predicted (F L 1) but many non-liquefied sites are cautioned ( ). Improvement of evaluation accuracy is in need. F L -method requires following information. N-value by standard penetration test (SPT) fine fraction content water level maximum design horizontal acceleration at surface earthquake magnitude F L >1 Liquefied sites Non-liquefied sites F L 1 53 35 24

25 Liquefaction (cont.) Japan s Building Standard Law does not require structural calculation for detached residence (residential land) Liquefaction risk is not evaluated Liquefaction measures are not required Show menus and leave selection to owners Development of affordable liquefaction evaluation method for residential land BRI tries possibility of SWS (Swedish weight sounding test), plus water level and soil judgment Development of practical techniques for residential land Applicability to existing house Prediction of subsidence

Tsunami wave force - Tentative guidelines for tsunami evacuation buildings - 26 Previous guidelines Partially relaxed current guidelines (tentative guidelines) Observed results by Tohoku Japan earthquake

Tsunami wave force (cont.) - Tentative guidelines for tsunami evacuation buildings - BRI, Kajima Co. and U. of Tokyo have carried out waterway experiments in order to develop (improve) CFD (Computational Fluid Dynamics) technique for evaluation of tsunami pressure on buildings. Improved CFD technique will be applied to evaluate the effects of openings, water infiltration, etc. AIJ discusses adding new chapter of tsunami loads on buildings into (Revised) Recommendations for Loads on Buildings in 214. 27 Waterway experiment Numerical simulation of Tsunami over seawall

Thank you for your kind attention. 28