Lesson 4-5: (P1) Dynamics of Vibration, Attenuation and Time History Flashcards
arise from sudden movements in a rupture zone in the Earth’s crust
seismic waves
the upper part of the building remains in delay in respect to the foundation moving, due to its _____; this causes strong vibrations of the structure with _____ between the structure and the ground and hence large inertial force arise
mass; resonance phenomena
due to _____, the soil is overloaded, becoming stiffer, hence producing change in its behavior
building’s weight
for stiff soils, the weight effect is to _____ the acceleration peak
reduce
for soft soils, possible to observe a relative _____ in acceleration peaks due to the presence of a building
increasing
part of the vibrating energy of buildings is released into soil through waves produced by buildings
soil effect
the severity of shaking is controlled primarily by two (2) factors:
- attenuation of ground motion
- earthquake characteristics
the dissipation of seismic energy as seismic waves move through layers of varying soil and rock strata
attenuation of ground motion
characterized as the decrease in amplitude of the seismic waves with distance from source
attenuation of ground motion
it results from geometric spreading of propagating waves, energy absorption and scattering of waves
attenuation of ground motion
during earthquake, different structures will behave differently
earthquake characteristics
seismic waves can be modified by site characteristics, earthquake characteristics and structural performance
earthquake characteristics
3 important earthquake measurement parameters that measure ground motions at the ground surface
- peak ground acceleration (PGA)
- peak ground velocity (PGV)
- peak ground displacement (PGD)
it has become the most popular parameter to denote the measure of an earthquake and has been related to the magnitude through several empirical relationship
peak ground acceleration (PGA)
these are essential for describing the important characteristics of strong ground motion in compact, quantitative form
ground motion parameters
the most common way of describing a ground motion is with time history
amplitude parameters
the peak ground acceleration (PGA) at a site depends not only on the magnitude and epicentral distance of the earthquake, but also on the _____
regional geological characteristics
as the PGA value decreases with the epicentral distance these empirical relationships are also called _____
attenuation laws
shaking depends on duration and frequency content, and to factors such as _____, _____, _____, and _____
length of fault rupture; focal depth; orientation of the fault; speed of rupture
large PGA earthquakes do not always create the most damage; in fact, a large PGA earthquake would produce _____ damage to some structures if it only occurs for a short time
little
shaking can be strengthen depending on the _____ along the path of the wave between the focus and the site, same as the _____ and _____
geologic conditions; soil conditions; topography
it is faster for hard rock than for soft soil
shear wave velocity
travel faster through hard rock than soft soil
seismic waves
local site characteristics greatly influence the seismic wave’s _____ and _____
frequency; amplitude
6 ground types based on shear-wave velocity to establish amplification effects for design purposes
- type A
- type B
- type C
- type D
- type E
- type F
this ground type is characterized by hard rock (igneous rock)
type A
this ground type is characterized by rock (volcanic rock)
type B