2 ce elec2 earthquake intro

49
CE ELEC2 EARTHQUAKE ENGINEERING MARK ELSON C. LUCIO, MSCE (Structures) Association of Structural Engineers of the Philippines (ASEP) Philippine Institute of Civil Engineers (PICE) American Society of Civil Engineers (ASCE) American Concrete Institute (ACI)

Upload: janus-antonio

Post on 20-Feb-2015

88 views

Category:

Documents


3 download

TRANSCRIPT

Page 1: 2 CE ELEC2 Earthquake Intro

CE ELEC2 EARTHQUAKE ENGINEERING

MARK ELSON C. LUCIO, MSCE (Structures)Association of Structural Engineers of the Philippines (ASEP)

Philippine Institute of Civil Engineers (PICE)American Society of Civil Engineers (ASCE)

American Concrete Institute (ACI)

Page 2: 2 CE ELEC2 Earthquake Intro

EARTHQUAKE

• An earthquake is manifested as ground shaking caused by the sudden release of energy in the Earth’s crust. This energy may originate from different sources, such as dislocations of the crust, volcanic eruptions, or even by man-made explosions.

Page 3: 2 CE ELEC2 Earthquake Intro

EARTHQUAKEFaults

Page 4: 2 CE ELEC2 Earthquake Intro

EARTHQUAKESource

Page 5: 2 CE ELEC2 Earthquake Intro

EARTHQUAKEIntensity

• Intensity is a non-instrumental measure of damage to structures, ground surface effects, e.g. fractures, cracks, landslides, and human reactions to earthquake shaking.

•It is a descriptive method which has been traditionally used to established earthquake size.

•It is a subjective damage evaluation measurement because of its qualitative nature, related to population density, familiarity with earthquake and type of constructions.

Page 6: 2 CE ELEC2 Earthquake Intro

EARTHQUAKEIntensity

Page 7: 2 CE ELEC2 Earthquake Intro

EARTHQUAKEMagnitude

• Magnitude is a quantitative measure of earthquake size and fault dimensions.

•It is therefore an instrumental, quantitative and objective scale.

•It can be used to quantify the amount of energy released during fault ruptures.

•Magnitude is proportional to the logarithm of seismic energy.

•The difference between two units of magnitude is a factor of 1,000 on energy release.

Page 8: 2 CE ELEC2 Earthquake Intro

EARTHQUAKEMagnitude

Page 9: 2 CE ELEC2 Earthquake Intro

EARTHQUAKEEffects

Page 10: 2 CE ELEC2 Earthquake Intro

EARTHQUAKEDamages

Page 11: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

• Model code: Uniform Building Code 1997 (UBC 97)

• Section 208 – Earthquake Loads

Page 12: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 13: 2 CE ELEC2 Earthquake Intro

WINDNSCP Chapter 2 – Minimum Design Loads

Page 14: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 15: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 16: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 17: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 18: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 19: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 20: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 21: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 22: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 23: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 24: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 25: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 26: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 27: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 28: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 29: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 30: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 31: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 32: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010Steel Braced Frames

Page 33: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 34: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 35: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 36: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 37: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 38: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 39: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 40: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 41: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 42: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 43: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 44: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 45: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 46: 2 CE ELEC2 Earthquake Intro

EARTHQUAKENSCP 2010

Page 47: 2 CE ELEC2 Earthquake Intro

EARTHQUAKE

• The Pacific Ring of Fire (or just The Ring of Fire) is an area where large numbers of earthquakes and volcanic eruptions occur in the basin of the Pacific Ocean. In a 40,000 km (25,000 mi) horseshoe shape, it is associated with a nearly continuous series of oceanic trenches, volcanic arcs, and volcanic belts and/or plate movements.

•The Ring of Fire has 452 volcanoes and is home to over 75% of the world's active and dormant volcanoes. It is sometimes called the circum-Pacific belt or the circum-Pacific seismic belt.

•About 90% of the world's earthquakes and 89% of the world's largest earthquakes occur along the Ring of Fire.

PACIFIC RING OF FIRE

Page 48: 2 CE ELEC2 Earthquake Intro

EARTHQUAKE

Countries

1. Chile2. Mexico3. United States4. Canada5. Russia6. Japan7. Philippines8. Japan9. New Zealand10. Antarctica

Page 49: 2 CE ELEC2 Earthquake Intro

Thank You!