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Reciprocity and power balance for partially coupled interfaces
Kees Wapenaar Evert Slob Jacob Fokkema Centre for Technical Geoscience Delft University of Technology
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Review of reciprocity theorems
Convolution type Correlation type Unified notation Acoustic Elastodynamic Electromagnetic Poroelastic Seismoelectric Review of boundary conditions Extension of reciprocity theorems Conclusions
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Review of reciprocity theorems
Convolution type Correlation type Unified notation Acoustic Elastodynamic Electromagnetic Poroelastic Seismoelectric Review of boundary conditions Extension of reciprocity theorems Conclusions
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A B A B ‘State A’ ‘State B’
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A B A B ‘State A’ ‘State B’
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‘State B’ ‘State A’ kA, rA kB, rB V n PB QB QA PA State A State B
PA, Vk,A QA,Fk,A kA, rA PB, Vk,B QB,Fk,B kB, rB Wave fields Sources Medium
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V n PB QB QA PA ‘State B’ ‘State A’
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‘State B’ ‘State A’ V n PB QB QA PA
Convolution-type reciprocity theorem: forward problems
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Review of reciprocity theorems
Convolution type Correlation type Unified notation Acoustic Elastodynamic Electromagnetic Poroelastic Seismoelectric Review of boundary conditions Extension of reciprocity theorems Conclusions
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‘State B’ ‘State A’ V n PB QB QA PA
Correlation-type reciprocity theorem
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‘State B’ ‘State A’ V n Q Q P P Power-flux through boundary
Power dissipated in medium Power radiated by sources
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‘State B’ ‘State A’ V n PB QB QA PA
Correlation-type reciprocity theorem: inverse problems
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Review of reciprocity theorems
Convolution type Correlation type Unified notation Acoustic Elastodynamic Electromagnetic Poroelastic Seismoelectric Review of boundary conditions Extension of reciprocity theorems Conclusions
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‘State B’ ‘State A’ V n PB QB QA PA
Convolution-type reciprocity theorem
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Unified notation (convolution type):
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Unified notation (convolution type):
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Unified notation (convolution type):
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Review of reciprocity theorems
Convolution type Correlation type Unified notation Acoustic Elastodynamic Electromagnetic Poroelastic Seismoelectric Review of boundary conditions Extension of reciprocity theorems Conclusions
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Acoustic: Poroelastic: Elastodynamic: Seismoelectric: Electromagnetic:
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‘State B’ ‘State A’ V n PB QB QA PA
Correlation-type reciprocity theorem
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V n PB QB QA PA ‘State B’ ‘State A’
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Unified notation (convolution type):
Unified notation (correlation type):
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Review of reciprocity theorems
Convolution type Correlation type Unified notation Acoustic Elastodynamic Electromagnetic Poroelastic Seismoelectric Review of boundary conditions Extension of reciprocity theorems Conclusions
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‘State B’ ‘State A’ n n V V PB QB QA PA Perfectly coupled interfaces:
No consequences for reciprocitytheorems of convolution type and correlation type Next: consider partially coupled interfaces
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Review of linear slip model
Displacement jump:
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Review of linear slip model of Schoenberg
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Review of linear slip model of Pyrak-Nolte et al.
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Review of linear slip model of Pyrak-Nolte et al.
Frequency domain
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Review of linear slip model of Pyrak-Nolte et al.
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Review of linear slip model
Schoenberg, Pyrak-Nolte et al: diagonal Nakagawa et al.: full matrix, with Generalization:
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Horizontal interface:
Arbitrary interface:
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Generalized boundary condition:
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Acoustic: Poroelastic: Elastodynamic: Seismoelectric: Electromagnetic:
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Review of reciprocity theorems
Convolution type Correlation type Unified notation Acoustic Elastodynamic Electromagnetic Poroelastic Seismoelectric Review of boundary conditions Extension of reciprocity theorems Conclusions
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n n V V PB QB QA PA ‘State B’ ‘State A’
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n n V V PB QB QA PA ‘State B’ ‘State A’
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‘State B’ ‘State A’ n n V V PB QB QA PA
Convolution-type reciprocity theorem: forward problems
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‘State B’ ‘State A’ n n V V PB QB QA PA
Correlation-type reciprocity theorem
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‘State B’ ‘State A’ n n V V Q P Q P Power-flux through boundary
Power dissipated in medium Power radiated by sources Power dissipated by interfaces
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‘State B’ ‘State A’ n n V V PB QB QA PA
Correlation-type reciprocity theorem: inverse problems
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Review of reciprocity theorems
Convolution type Correlation type Unified notation Acoustic Elastodynamic Electromagnetic Poroelastic Seismoelectric Review of boundary conditions Extension of reciprocity theorems Conclusions
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Unified reciprocity theorems have been formulated
of the convolution and correlation type
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Unified reciprocity theorems have been formulated
of the convolution and correlation type Valid for acoustic, elastodynamic, electromagnetic, poroelastic and seismoelectric waves
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Unified reciprocity theorems have been formulated
of the convolution and correlation type Valid for acoustic, elastodynamic, electromagnetic, poroelastic and seismoelectric waves Boundary condition for imperfectly coupled interface:
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Unified reciprocity theorems have been formulated
of the convolution and correlation type Valid for acoustic, elastodynamic, electromagnetic, poroelastic and seismoelectric waves Boundary condition for imperfectly coupled interface: No effects on source-receiver reciprocity
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Unified reciprocity theorems have been formulated
of the convolution and correlation type Valid for acoustic, elastodynamic, electromagnetic, poroelastic and seismoelectric waves Boundary condition for imperfectly coupled interface: No effects on source-receiver reciprocity Imaginary part of accounts for dissipation by interfaces
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