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Use of numerical modelling to identify the transfer function and application to the geostatistical procedure in the solution of inverse problems in groundwater
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I. Butera
Veröffentlicht/Copyright:
2006
The restoring of the pollutant release history makes use of transfer functions (TFs) usually known by analytical formulation. In many cases the computation of an analytical TF is not possible; this fact limits the application of the inverse procedures to very simple conditions or it forces to drastic simplifications of complicated problems. In this paper a new procedure, useful to compute the numerical transfer functions in transport problems with no analytical solution, is outlined. This method, analogous to the computation of the Instantaneous Unit Hydrograph (IUH) in surface hydrology, makes use of mathematical modelling.
Published Online: --
Published in Print: 2006-09-01
Copyright 2006, Walter de Gruyter
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Artikel in diesem Heft
- Inverse doping problems for a P-N junction
- Use of numerical modelling to identify the transfer function and application to the geostatistical procedure in the solution of inverse problems in groundwater
- Newton–Lavrentiev regularization of ill-posed Hammerstein type operator equation
- Two-step regularization methods for linear inverse problems
- Tomography problem for the polarized-radiation transfer equation
- Optimal control for singular equation with nonsmooth nonlinearity
- Monotonicity based imaging methods for elliptic and parabolic inverse problems
Artikel in diesem Heft
- Inverse doping problems for a P-N junction
- Use of numerical modelling to identify the transfer function and application to the geostatistical procedure in the solution of inverse problems in groundwater
- Newton–Lavrentiev regularization of ill-posed Hammerstein type operator equation
- Two-step regularization methods for linear inverse problems
- Tomography problem for the polarized-radiation transfer equation
- Optimal control for singular equation with nonsmooth nonlinearity
- Monotonicity based imaging methods for elliptic and parabolic inverse problems
