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A bit more about
The Domain Reduction Method
Boris Jeremić
Professor, University of California, Davis
Faculty Scientist, Lawrence Berkeley National Laboratory, Berkeley
Ottawa Workshop 2010
Jeremić
A bit more about The Domain Reduction Method
The Domain Reduction Method (DRM)
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Work by Bielak et al. (2003) at CMU.
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Features:
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General 3D seismic input (p, s, Love, Rayleigh waves...)
Nonlinear (elastic-plastic) ESSI
Minimal outgoing waves, only radiation of NPPSSS energy
Consistent replacement for seismic moment released from
hypocenter with forces on a single layer of element around
NPPSSS
Jeremić
A bit more about The Domain Reduction Method
DRM
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A large physical domain is to be analyzed for dynamic
behavior.
The source of disturbance is a known time history of a
force field Pe (t).
That source of loading is far away from a local feature
which is dynamically excited by Pe (t)
Local feature
Ω
ui
ub
Pe (t)
Ω+
Γ
ue
Large scale domain
Jeremić
A bit more about The Domain Reduction Method
DRM
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remove local feature, create a free field model
domain inside the boundary Γ is named Ω0 .
outside boundary Γ, is Ω+ .
outside domain Ω+ is the same as in the original model,
simplification, is done on the domain inside boundary Γ.
u0i
Ω0
u0b
Pe (t)
Ω
+
Γ
u0e
Simplified large scale domain
Jeremić
A bit more about The Domain Reduction Method
DRM
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Equations of motions for a complete system
M
ü
Jeremić
A bit more about The Domain Reduction Method
+
K
u
=
Pe
DRM
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Eq of motions written for each subdomain (interior,
boundary and exterior of Γ)


MiiΩ
MibΩ
0
 üi 
 M Ω M Ω + M Ω+ M Ω+ 
ü
+
bi
bb
bb
be
 b 
Ω+
Ω+
üe
0
Meb
Mee
 


Ω
Kib
0
 ui   0 
Ω + K Ω+ K Ω+ 
u
0
Kbb
=
bb
be
 b  

Ω+
Ω+
ue
Pe
Keb
Kee

KiiΩ
 KΩ
bi
0

Jeremić
A bit more about The Domain Reduction Method
DRM
Separate previous equation into two domains Ω and Ω+
MiiΩ MibΩ
Ω
MbiΩ Mbb
Ω+
Ω+
Mbb
Mbe
Ω+
Ω+
Meb Mee
üi
üb
+
KiiΩ KibΩ
Ω
KbiΩ Kbb
üb
üe
+
Ω+
Ω+
Kbb
Kbe
Ω+
Ω+
Keb Kee
ui
ub
=
ub
ue
For this separation to work one needs to enforce
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compatibility of displacements
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equilibrium (through action–reaction forces Pb )
Jeremić
A bit more about The Domain Reduction Method
0
Pb
=
,Ω
−Pb
Pe
,
DRM
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Simplified interior domain without local feature (with ui0 , ub0 ,
ue0 and Pb0 )
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The equations of motion in Ω+ for the auxiliary problem
can now be written as:
Ω+
Ω+
Mbb
Mbe
Ω+
Ω+
Meb
Mee
üb0
üe0
Jeremić
A bit more about The Domain Reduction Method
+
Ω+
Ω+
Kbb
Kbe
Ω+
Ω+
Keb
Kee
ub0
ue0
=
−Pb0
Pe
DRM
Use second part of previous equation to obtain the dynamic
force Pe as
Ω+ 0
Ω+ 0
Ω+ 0
Ω+ 0
Pe = Meb
üb + Mee
üe + Keb
ub + Kee
ue
Jeremić
A bit more about The Domain Reduction Method
DRM
The total displacement, ue , can be expressed as the sum of the
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free field ue0 (from the background, simplified model, free
field), and
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the residual field we (comming from the local feature)
ue = ue0 + we
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this is a change of variables and not superposition!
Jeremić
A bit more about The Domain Reduction Method
DRM
By substitution into full equation one gets


MiiΩ
MibΩ
0
üi


 M Ω M Ω + M Ω+ M Ω+ 
ü
+
bi
bb
bb
be
 0 b

Ω+
Ω+
üe + ẅe
0
Meb
Mee
 


KibΩ
0
ui

  0 
Ω + K Ω+ K Ω+ 
u
0
Kbb
=
bb
be
 0 b
 

Ω+
Ω+
P
u
+
w
Keb
Kee
e
e
e

KiiΩ
 KΩ
bi
0

Jeremić
A bit more about The Domain Reduction Method
DRM
After moving the free field motions ue0 to the right hand side,
prevous equation becomes


MiiΩ
MibΩ
0
 üi 
 M Ω M Ω + M Ω+ M Ω+ 
ü
+
bi
bb
bb
be
 b 
Ω+
Ω+
ẅ
0
Meb
Mee
e

 Ω

Ω
Kii
Kib
0
 ui 
 K Ω K Ω + K Ω+ K Ω+ 
u
=
bi
bb
bb
be
 b 
Ω+
Ω+
we
0
Keb
Kee


0


Ω+ 0
Ω+ 0
−Mbe
üe − Kbe
ue


Ω+ 0
Ω+ 0
−Mee
üe − Kee
ue + Pe

Jeremić
A bit more about The Domain Reduction Method
DRM
By substitution of Pe


MiiΩ
MibΩ
0
 üi 
 M Ω M Ω + M Ω+ M Ω+ 
ü
+
bi
bb
be
bb
 b 
Ω+
Ω+
ẅ
0
Meb
Mee
e

 Ω

Ω
Kii
Kib
0
 ui 
 K Ω K Ω + K Ω+ K Ω+ 
u
=
bi
bb
bb
be
 b 
Ω+
Ω+
we
0
Keb
Kee


0


Ω+ 0
Ω+ 0
−Mbe
üe − Kbe
ue

Ω+ 0
Ω+ 0 
Meb
üb + Keb
ub

Jeremić
A bit more about The Domain Reduction Method
DRM
The right hand side is the dynamically consistent replacement
force (so called effective force, P eff ) for the dynamic source
forces Pe .
P eff
 eff  

0
 Pi  

Ω+ 0
Ω+ 0
−Mbe
üe − Kbe
ue
=
=
Pbeff
 eff  
Ω+ 0
Ω+ 0 
Pe
Meb
üb + Keb
ub
Jeremić
A bit more about The Domain Reduction Method
DRM
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Seismic forces Pe replaced by P eff
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P eff applied only to a single
layer of elements next to Γ.
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Only outgoing waves from
dynamics of the NPP
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Material inside Ω
can be elastic-plastic
Ω
Γe
A bit more about The Domain Reduction Method
ue
+
Ω
Pe
Jeremić
Γ
ub
Fault
ui
ue
Γ
+
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