This paper deals with time-domain surface-impedance boundary conditions in computational magnetodynamics considering two dual finite-element formulations and a nonlinear magnetic constitutive law. Based on the resolution of the 1-D eddy-current problem in a semi-infinite slab, the massive conducting region is accounted for by choosing a number of exponentially decreasing trigonometric basis functions covering the relevant frequency range of the application in hand. Herein the method is elaborated for the magnetic-vector- potential formulation and the magnetic-field formulation. Results for both formulations are compared and validated on 2-D linear and nonlinear test cases.status: publishe
In several electromagnetic applications field quantities are confined in layers which are thin with ...
The authors propose a novel time-domain extension of the well-known frequency-domain surface-impedan...
In several electromagnetic applications, field quantities are confined in layers that are thin with ...
This paper deals with time-domain surface-impedance boundary conditions in computational magnetodyna...
This paper deals with time-domain surface-impedance boundary conditions in computational magnetodyna...
peer reviewedThis paper deals with time-domain surface-impedance boundary conditions in computationa...
The authors propose a novel time-domain extension of the well-known frequency-domain surface-impedan...
The authors propose a novel time-domain extension of the well-known frequency-domain surface-impedan...
This paper deals with time-domain surface-impedance boundary conditions in computational magnetodyna...
peer reviewedThe authors propose a novel nonlinear time-domain extension of the well-known frequency...
In computational magnetodynamics, surface impedance boundary conditions allow to accurately account ...
In computational magnetodynamics, surface impedance boundary conditions allow to accurately account ...
In computational magnetodynamics, surface impedance boundary conditions allow to accurately account ...
In several electromagnetic applications field quantities are confined in layers which are thin with ...
In several electromagnetic applications field quantities are confined in layers which are thin with ...
In several electromagnetic applications field quantities are confined in layers which are thin with ...
The authors propose a novel time-domain extension of the well-known frequency-domain surface-impedan...
In several electromagnetic applications, field quantities are confined in layers that are thin with ...
This paper deals with time-domain surface-impedance boundary conditions in computational magnetodyna...
This paper deals with time-domain surface-impedance boundary conditions in computational magnetodyna...
peer reviewedThis paper deals with time-domain surface-impedance boundary conditions in computationa...
The authors propose a novel time-domain extension of the well-known frequency-domain surface-impedan...
The authors propose a novel time-domain extension of the well-known frequency-domain surface-impedan...
This paper deals with time-domain surface-impedance boundary conditions in computational magnetodyna...
peer reviewedThe authors propose a novel nonlinear time-domain extension of the well-known frequency...
In computational magnetodynamics, surface impedance boundary conditions allow to accurately account ...
In computational magnetodynamics, surface impedance boundary conditions allow to accurately account ...
In computational magnetodynamics, surface impedance boundary conditions allow to accurately account ...
In several electromagnetic applications field quantities are confined in layers which are thin with ...
In several electromagnetic applications field quantities are confined in layers which are thin with ...
In several electromagnetic applications field quantities are confined in layers which are thin with ...
The authors propose a novel time-domain extension of the well-known frequency-domain surface-impedan...
In several electromagnetic applications, field quantities are confined in layers that are thin with ...