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Time-domain staggered-grid finite-difference simulation of GPR data
How Wei Chen, Tai Min Huang
Department of Earth Sciences
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peer-review
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Scopus citations
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Dive into the research topics of 'Time-domain staggered-grid finite-difference simulation of GPR data'. Together they form a unique fingerprint.
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Keyphrases
Radar Data
100%
Ground Penetrating Radar
100%
Finite Difference Simulation
100%
Staggered-grid Finite-difference
100%
Absorbing Boundary
66%
Spatial Derivatives
33%
Numerical Methods
33%
Electrical Conductivity
33%
Electric Permittivity
33%
Electrical Properties
33%
TE Mode
33%
CA Model
33%
Second-order Difference
33%
Fourth Order
33%
Absorption Mechanism
33%
Common Source
33%
Temporal Derivatives
33%
Synthetic Instances
33%
Operating Frequency
33%
Finite-difference Time-domain
33%
Attenuation Coefficient
33%
Attenuation Properties
33%
Paraxial Approximation
33%
Magnetic Permeability
33%
Earth Materials
33%
Radar Wave Propagation
33%
First Order Effects
33%
One-way Wave Equation
33%
Permeability Loss
33%
Loss Tangent
33%
Frequency-dependent Attenuation
33%
Absorbing Boundary Conditions
33%
Domain Boundary
33%
Artificial Damping
33%
Staggered Grid Technique
33%
Value Coefficients
33%
Time-marching Schemes
33%
Two-dimensional Medium
33%
Zero Offset
33%
Damping Mechanism
33%
Engineering
Time Domain
100%
Radar Data
100%
Finite Difference Method
100%
Grid Point
50%
Operating Frequency
50%
Two Dimensional
50%
Significant Change
50%
Fourth Order
50%
Relative Velocity
50%
Loss Tangent
50%
Digital Ground
50%
Domain Boundary
50%
Dependent Attenuation
50%
Electrical Conductivity
50%
Magnetic Permeability
50%
Boundary Condition
50%
Physics
Finite Difference Method
100%
Ground Penetrating Radar
100%
Absorbing Boundary
100%
Wave Equation
33%
Boundary Condition
33%
Wave Propagation
33%
Magnetic Permeability
33%
Permittivity
33%
Mathematical Method
33%
Attenuation Coefficient
33%
Loss Tangent
33%
Earth Surface
33%
Electrical Resistivity
33%
Electrical Property
33%
Earth and Planetary Sciences
Radar Data
100%
Finite Difference Method
100%
Ground Penetrating Radar
100%
Near-Surface Geology
33%
Mathematical Method
33%
Diffraction
33%
Boundary Condition
33%
Permittivity
33%
Magnetic Permeability
33%
Electrical Resistivity
33%
Attenuation Coefficient
33%
Time Marching
33%
Wave Equation
33%
Electrical Property
33%