Electromagnetic fields in magnetic resonance imaging, groundwater flows, charge carriers in semiconductors and numerous further spatially distributed physical processes have one thing in common: they can be modeled by means of partial differential equations. The solution for such complex mathematical equations can usually not be obtained as a mathematical formula. Therefore, computer-based approximation methods are applied. In order to calculate these, the respective spatial domain must be divid...
Electromagnetic fields in magnetic resonance imaging, groundwater flows, charge carriers in semiconductors and numerous further spatially distributed physical processes have one thing in common: they can be modeled by means of partial differential equations. The solution for such complex mathematical equations can usually not be obtained as a mathematical formula. Therefore, computer-based approximation methods are applied. In order to calculate these, the respective spatial domain must be divid...
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