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)
2
Q
intensity
A
- measure of the effects of an earthquake on people and infrastructure
3
Q
magnitude
A
- amount of energy released during an earthquake
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
5
Q
frequency of different terrains
A
- soil = <1 Hz
- hard rock = >1Hz
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
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
8
Q
elastic limit
A
- material exhibit elastic behavior
- beyond elastic limit there are two scenarios:
- material fails immediately
- plastic deformation
9
Q
flexibility of buildings
A
`- 10 Hz/ number of storeys
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
11
Q
faults
A
- complex zones of breakage
- rough interlocking rocks
12
Q
fault rupture
A
- initiated at hypocenter
- the initiation of an earthquake
13
Q
slip fault
A
- displacement between the two rock blocks
14
Q
seismic waves
A
- caused by the release of energy in the earth
15
Q
amplitude
A
- max value measured from the equilibrium
- attuation: loss in amplitude as the wave propagates away from its source
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