ATTENUATION Flashcards
It is the reduction of the force, effect, or
value of something
Attenuation
It is the reduction in the amplitude of seismic waves
as they travel away from the earthquake source
Attenuation
describes the energy loss
experienced by seismic waves as they propagate. It is
controlled by the temperature, composition, melt
content, and volatile content of the rocks through
which the waves travel
Seismic attenuation
FACTORS AFFECTING
ATTENUATION
Distance from Epicenter
Geological Conditions
Frequency of Seismic Waves
The attenuation of seismic waves is due
to three effects:
Geometrical Spreading
Absorption (anelastic attenuation)
Scattering (elastic attenuation)
PROCESS WHERE Seismic wave amplitudes vary as they travel
across the Earth.
Geometrical Spreading
This is the energy loss due to anelastic processes or internal friction
during wave propagation.
Absorption
is an important factor caused by the
heterogeneity of the Earth’s crust and
mantle and availability of hydrocarbon
reservoirs.
Scattering (elastic attenuation)
Three Types of Scattering
Rayleigh Scattering
Mie Scattering
Non-Selective Scattering
This occurs when seismic waves encounter small,
rough surfaces or irregularities in the medium.
Rayleigh Scattering
This type happens when the wavelength of the seismic
waves is comparable to the size of the scattering particles or structure.
Mie Scattering
This occurs when waves scatter off larger,
heterogenous structures in the medium, regardless of their wavelength.
Non-Selective Scattering
Part of the total energy that is radiated away and causes
shaking
SEISMIC ENERGY