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4 th International Conference on Rehabilitation and Maintenance in Civil Engineering Building evaluation using two components of acceleration time histories causes by shallow crustal fault earthquakes with maximum magnitude 7 Mw Windu Partono,


  1. 4 th International Conference on Rehabilitation and Maintenance in Civil Engineering Building evaluation using two components of acceleration time histories causes by shallow crustal fault earthquakes with maximum magnitude 7 Mw Windu Partono, Masyhur Irsyam, Indrastono Dwi Atmanto, Andi Retno Ari Setiaji, Sigit Purnomo and Robby Yanuar Setiawan

  2. Introduction ➢ Fault is one of the dangerous earthquake sources that can cause building failure. A lot of buildings were collapsed caused by Yogyakarta fault (2006) and Pidie fault (2016) source earthquakes with maximum magnitude 6.4 Mw. ➢ Based on the research conducted by Team for Revision of Seismic Hazard Maps of Indonesia 2010 and National Center for Earthquake Studies (PUSGEN) 2017, Lasem fault and Semarang fault are two earthquake sources crosses Semarang.

  3. Introduction

  4. Introduction ➢ Stability analysis of a structure can be evaluated by conducting seismic loads. The objective of the analysis is to get the information of maximum loads that can be applied to a structure. ➢ The stability analysis in this study were implemented for 3 buildings (minimum 40 m height) at Semarang by conducting dynamic structural analysis and applying modified acceleration time histories. ➢ The modified acceleration time histories were developed from earthquake scenarios caused by Semarang fault earthquakes with magnitude 6 -7 Mw.

  5. Research Methodology 1. Collecting information and data related with – structural details – geological and geotechnical data – positions of each building against seismic source – acceleration time histories due to shallow crustal fault sources with magnitude 6 – 7 Mw and maximum distance 30 km. 2. Developing modified acceleration time histories by conducting response spectral matching analysis . 3. Conducting shear wave propagation analysis using modified time histories for developing surface acceleration time histories 4. Performing dynamic structural analysis to get the deformation and drift ratio of buildings due to acceleration time histories and surface spectra developed from SNI:1726-2012.

  6. Data Requirements (building information) Distance Height of Depth of to Building Dimension Site Building Bedrock Seismic Number Plans (m) Class (m) (m) Source (Km) B1 22x78 48.73 SE 165 3.13 (Hospital) B3 (Hotel) 28.8x19.75 41.2 SC 40 0.65 B8 (University 40.75x16.2 43.2 SD 60 4.98 Building)

  7. Data Requirements (building position)

  8. Data Requirements (structural details) +43.20 +39.40 +35.60 +31.80 Plan, elevation, materials and detail +28.0 of element structure +24.50 H 43/20 m +21.0 +17.50 2.07 m +14.0 3.65 m +10.50 +7.0 4.7 m +3.0 3.65 m 8 m 8 m 8 m 2.07 m Building B3 2.07 m 2.07 m 8 m 8 m 8 m

  9. Data Requirements (geotechnical data) V S30 data Site Class data Boring investigation

  10. Data Requirements (Bedrock Measurement) Hammer Data Logger and Computer Seismometer GPS 10

  11. Data Requirements (Bedrock Measurement) Bedrock Elevation Bedrock elevation map

  12. Data Requirements (acceleration time histories) Earthquake Station and Epicentre Distance Magnitude Events (km) (Mw) Chuetsu-oki Nagaoka (3.98) and Joetsu 6.8 Japan Kakizakiku Kakizaki (9.43) IWTH24 (3.1), Mizusawaku Iwate_ Japan Interior O Ganecho (7.82) and 6.9 IWTH24 (11.68) Cambria - Hwy 1 Caltrans Bridge San Simeon_ (5.07) and Templeton - 1-story 6.52 CA Hospital (6.97) Northridge-02 Newhall - Fire Sta (7.36) and 6.05 California Pacoima Kagel Canyon (6.61) All acceleration time histories (reverse mechanism earthquake) were collected from PEER NGA-West 2 Databases

  13. Data Requirements (acceleration time histories) Original Acceleration Time Histories of San Simeon earthquake 6.52 Mw with epicentre distance 6.97 Km collected from PEER NGA-West 2 Databases San Simeon 6.52 Mw 6.97 Km 0.5 NS Direction 0.4 EW direction 0.3 0.2 Acceleration (g) 0.1 0 -0.1 -0.2 -0.3 -0.4 -0.5 0 2 4 6 8 10 12 14 16 18 20 Time (sec)

  14. Data Requirements (surface spectra SNI:1726-2012) Surface spectra and design spectra from SNI-2012 at building B3 location (SD site class) Spectra TC Undip (B3) - SD 1.4 Surface Spectra 1.2 Design Spectra Acceleration (g) 1 0.8 0.6 0.4 0.2 0 0 0.5 1 1.5 2 2.5 3 3.5 4 Periods (s)

  15. Data Analysis (Response Spectral Matching) Response Spectra Target (Deterministic Seismic Hazard Analysis) Spectral Target for building B3 (SD site class) Three atenuation functions for deterministic seismic hazard analysis (Boore and Atkinson , 2008, Campbell and Bozorgnia, 2008 and Chiou, and Youngs, 2008) Spectral Target Horizontal (N-S and E-W Directions) 0.9 0.8 Chi-Chi 5.72 Km Chi-Chi 8.34 Km 0.7 Acceleration (g) San Simeon 5.07 Km 0.6 San Simeon 6.97 Km 0.5 Iwate 7.82 Km 0.4 Iwate 11.68 Km 0.3 Iwate 13.07 Km 0.2 0.1 0 0 0.5 1 1.5 2 2.5 3 3.5 4 Period (sec)

  16. Data Analysis (Response Spectral Matching) Fault Select Ground Motion in Terms of Acceleration Time Histories For Scenario M and R Spectral Modified Ground Matching motion Analysis due to Lasem Fault Calculate Target Spectral for specific earthquake M1 and R1

  17. Data Analysis (Response Spectral Matching) Response Spectral Matching San Simeon 6.52 Mw, 6.97 Km San Simeon 6.52 Mw 6.97 Km 0.5 NS Direction 0.4 EW direction 0.3 0.2 Acceleration (g) 0.1 0 -0.1 -0.2 -0.3 -0.4 -0.5 0 2 4 6 8 10 12 14 16 18 20 Time (sec) Original acceleration time histories

  18. Data Analysis (Response Spectral Matching) Response Spectral Matching San Simeon 6.52 Mw, 6.97 Km Matched Acceleration Time Histories San Simeon 6.52 Mw 6.97 Km 0.3 N-S Direction 0.2 E-W Direction 0.1 Acceleration (g) 0 -0.1 -0.2 -0.3 -0.4 -0.5 0 2 4 6 8 10 12 14 16 18 20 Time (sec) Matched / modified acceleration time histories

  19. Data Analysis (Site Response/Propagation Analysis) H Acceleration Time Histories at Building Acceleration Ground Time Histories Surface at the Surface Propagation Soil Deposits Analysis Acceleration time histories at the bedrock Bedrock elevation) Modified from Irsyam 2015

  20. Data Analysis (Response Spectral Matching) Response Spectral Matching San Simeon 6.52 Mw, 6.97 Km Surface Acceleration Time Histories San Simeon 6.52 Mw 6.97 Km 0.15 N-S Direction 0.1 E-W Direction 0.05 Acceleration (g) 0 -0.05 -0.1 -0.15 0 2 4 6 8 10 12 14 16 18 20 Time (sec) Propagating of modified acceleration time histories for producing surface acceleration time histories

  21. Structural Analysis 1.00 Chuetsu-Oki NS Chuetsu-Ok1 EW 0.80 Iwate NS 0.60 Iwate EW Acceleration (g) Northridge-02 NS 0.40 Northridge-02 EW 0.20 San Simeon NS 0.00 San Simeon EW 0.00 1.00 2.00 3.00 4.00 SNI 2012 Spectra T (sec) 50 Chuetsu-Oki 9.43 km 40 Iwate 7.82 km Floor Elevation (m) 30 Northridge-02 6.61 km 20 San Simeon 6.97 km 10 SNI 2012 (Y Direction) 0 SNI 2012 (X Direction) 0.00% 0.10% 0.20% 0.30% 0.40% 0.50% Drift Ratio Comparison of spectral acceleration calculated from SNI-03-1726-2012 and two components acceleration time histories of four earthquake events (a) and drift ratio of building B1 when subjected to SNI-03-1726-2012 spectral acceleration and acceleration time histories of four earthquake events

  22. Structural Analysis 0.80 Chuetsu-Oki NS Chuetsu-Ok1 EW 0.60 Iwate NS Iwate EW Acceleration (g) 0.40 Northridge-02 NS Northridge-02 EW 0.20 San Simeon NS San Simeon EW 0.00 0.00 1.00 2.00 3.00 4.00 SNI 2012 Spectra T (sec) 50 Chuetsu-Oki 9.43 Km 40 Iwate 11.68 Km Floor Elevation (m) 30 Northridge-02 6.61 km San Simeon 6.97 km 20 SNI 2012 (Y Direction) 10 SNI 2012 (X Direction) 0 0.00% 0.05% 0.10% 0.15% 0.20% 0.25% 0.30% Drift Ratio Comparison of spectral acceleration calculated from SNI-03-1726-2012 and two components acceleration time histories of four earthquake events (a) and drift ratio of building B1 when subjected to SNI-03-1726-2012 spectral acceleration and acceleration time histories of four earthquake events

  23. Structural Analysis Results 50 Chuetsu-Oki 9.43 Km 40 Iwate 11.68 Km Floor Elevation (m) 30 Northridge-02 6.61 km San Simeon 6.97 km 20 SNI 2012 (Y Direction) 10 SNI 2012 (X Direction) 0 0.00% 0.05% 0.10% 0.15% 0.20% 0.25% 0.30% Drift Ratio Drift ratio of building B1

  24. Structural Analysis Results 50 Chuetsu-Oki 9.43 Km 40 Floor Elevation (m) Iwate 7.82 Km 30 Northridge-02 6.61 Km 20 San Simeon 6.97 kM 10 SNI 2012 (Y Direction) 0 SNI 2012 (X Direction) 0.00% 0.10% 0.20% 0.30% 0.40% Drift Ratio Drift ratio for building B2

  25. Structural Analysis Results 50 Chuetsu-Oki 9.43 Km Floor Elevation (m) 40 Iwate 11.68 Km 30 Northridge-02 6.61 Km San Simeon 6.97 Km 20 SNI 2012 (Y Direction) 10 SNI 2012 (X Direction) 0 0.00% 0.20% 0.40% 0.60% 0.80% Drift Ratio Drift ratio for building B3

  26. CONCLUSIONS 1. Stability performance of buildings can be predicted by evaluating surface response spectra calculated using seismic code and surface response spectra calculated from acceleration time histories from a specific earthquake event. If the surface response spectra calculated using seismic code is greater than the surface response spectra calculated from acceleration time histories the structure will strong enough to resist the earthquake force. 26

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