numerical modeling of seismic wave processes using grid...
TRANSCRIPT
![Page 1: Numerical modeling of seismic wave processes using grid ...novikov/miptip16/slides/favorskaya.pdf · Numerical modeling of seismic wave processes using grid-characteristic method](https://reader030.vdocument.in/reader030/viewer/2022040817/5e6240ca0c09ae624814caf1/html5/thumbnails/1.jpg)
Numerical modeling of seismic wave
processes using grid-characteristic method
Dr Alena V. Favorskaya
Moscow Institute of Physics and Techology [email protected]
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Contents
We will discuss shelf seismic exploration We will prove the following thesisThe use of elastic wave modeling is more better than the use of acoustic wave modeling for shelf seismic exploration independently on the source-receivers system type.
Also we will discuss another applications of elastic waves modeling: Numerical modeling of Arctic problems Numerical simulation in geology Numerical modeling of seismic stability
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Shelf seismic exploration
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Types of source-receivers systems
Streamer• P-waves• Low price• High performance• Use of acoustic wave
modeling?
Seabed stations• P-, S-, PS-, SP-waves• High price• High comprehension of
obtained data• Use of elastic wave
modeling only
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Comparison between acoustic and elastic waves modeling
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horizontal component vertical component
Comparison between acoustic and elastic waves modeling
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Numerical modeling of Arctic problems
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Destruction of the iceberg underintense dynamic impacts
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Numerical simulation in
geology
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Types of cracks: barriers, conductors and neutral one
K = 1.0 (no
cracks)
K = 0.9
K = 0.5
K = 0.6
K = 0.75
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Numerical modeling of seismic stability
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Seismic stability of the buildings
1000 m 2000 m 3000 m 4000 mDifferent depth of earthquake hypocenter
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Thank you for your attention!
We discussed: Shelf seismic explorationThe use of elastic wave modeling is more better than the use of acoustic wave modeling for shelf seismic exploration independently on the source-receivers system type.
Also we discussed another applications of elastic waves modeling: Numerical modeling of Arctic problems Numerical simulation in geology Numerical modeling of seismic stability
![Page 14: Numerical modeling of seismic wave processes using grid ...novikov/miptip16/slides/favorskaya.pdf · Numerical modeling of seismic wave processes using grid-characteristic method](https://reader030.vdocument.in/reader030/viewer/2022040817/5e6240ca0c09ae624814caf1/html5/thumbnails/14.jpg)
Appendix:Grid-characteristic
method
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System of equations describing elastic and acoustic waves
density, velocity in the elastic media, stress tension, Lame’s parameters,
speed of P-waves,
speed of S-waves.
т
tv σv
т
t v v v σ Iv v v
vv
σ,
Elastic waves:
density, velocity in the acoustic media, pressure, speed of sound.
tv p v
2t pс v v
vv
p c
Acoustic waves:
1 22pc
1 2
sc
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Given traction
Given velocity of boundary
Mixed boundary conditionsAbsorbing boundary contions
Boundary Interface
p fσrr
v Vrr
Continuity of the velocity and traction
Free sliding conditions
The interface condition between acoustic and elastic bodies
,a b a bv v V rr r r r
, , 0a b a b
a b p pv p v p r r r r
Boundary and interface conditions