Lecture 5+6 Flashcards

1
Q

the Mercalli intensity scale

A
  • method of measuring intensity of earthquakes
  • based on observable earthquake damage
  • not necessarily accurate (eyewitness accounts aren’t reliable)
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2
Q

intensity

A
  • measure of the effects of an earthquake on people and infrastructure
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3
Q

magnitude

A
  • amount of energy released during an earthquake
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4
Q

shake map

A
  • intensity map generated automatically in near - real time using data from seismograph stations
  • input : ground motion data; knowledge of regional geology
  • output: computed intensity
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5
Q

frequency of different terrains

A
  • soil = <1 Hz
  • hard rock = >1Hz
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6
Q

resonance

A
  • a system experience a very large oscillations when it is disturbed by a forcing function of frequency equal to its natural frequency
  • the energy of the forcing function is added to the system so that oscillations are reinforced
  • oscillations grow bigger until the object breaks
  • The oscillation caused by a seismic wave
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7
Q

liquefaction

A
  • the strength of soil is reduced by rapid and violent shaking or loading
  • occurs in saturated soils in which the space between articles is filled with water
  • low pore pressure = strong binding force
  • high pore pressure = weak binding force
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8
Q

elastic limit

A
  • material exhibit elastic behavior
  • beyond elastic limit there are two scenarios:
  • material fails immediately
  • plastic deformation
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9
Q

flexibility of buildings

A

`- 10 Hz/ number of storeys

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10
Q

resonance

A
  • seismic waves act as forcing functions on foundation materials and buildings
  • the building resonance is the number of seconds it takes for he building to naturally vibrate back and forth
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11
Q

faults

A
  • complex zones of breakage
  • rough interlocking rocks
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12
Q

fault rupture

A
  • initiated at hypocenter
  • the initiation of an earthquake
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13
Q

slip fault

A
  • displacement between the two rock blocks
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14
Q

seismic waves

A
  • caused by the release of energy in the earth
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15
Q

amplitude

A
  • max value measured from the equilibrium
  • attuation: loss in amplitude as the wave propagates away from its source
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16
Q

period

A
  • time between two successive crests
17
Q

frequency

A
  • number of waveforms in 1 second
18
Q

wavelength

A
  • distance between two successive crests
19
Q

propagation

A
  • velocity of propagation: v(m/s) = L(m/s)/T(s)
20
Q

seismometer

A
  • sensor that detects ground motion
21
Q

seismograph

A

an instrument that record ground motion

22
Q

siesmogram

A
  • paper record or digital file with data describing ground motion
23
Q

Zhang Heng

A
  • first seismograph in china
24
Q

Body waves

A
  • propagate through the whole body of the earth
  • Large earthquakes generate body waves recorded all over the world
25
Q

P waves

A
  • primary waves
  • compressional energy
  • small amplitude
  • travel fastest: frist to be recorded
  • faster in water slower in hard rock
26
Q

s waves

A
  • secondary waves
  • shear energy
  • larger amplitude
  • don’t travel as fast
27
Q

surface waves

A
  • low frequency
  • slow velocity
  • very large amplitudes
28
Q

Richter magnitude scale

A
  • difference between S and P wave arrival times
  • max amplitude of body waves
  • logarithmic scale (when the amplitude is multiplied by a factor of 10 the magnitude increases by +1