Add to ORKGThe Authors suggest an approximate approch for the solution of the problem of the identification of transmissivity in porous ground: they suppose transmissivity is steady comparent to gradient bat not to divergence. We show a numeric example concerning the groundwater flow of the Low Esino Basin (Ancona - Italy
The identification of the transmissivity, T, of a confined aquifer, for which the 2D flow condition ...
The paper deals with the identification of unknown storativity and transmissiv-ity distributions wit...
International audienceThe paper deals with the identification of unknown storativity and transmissiv...
The Authors suggest an approximate approch for the solution of the problem of the identification of ...
The Authors suggest an approximate approch for the solution of the problem of the identification of ...
The Authors suggest an approximate approch for the solution of the problem of the identification of ...
This paper is devoted to the inverse problem of identifying a spatially varying coefficient in a lin...
The differential system (DS) method for the identification of transmissivity and storativity is appl...
This paper is devoted to the inverse problem of identifying a spatially varying coefficient in a lin...
AbstractWe discuss the numerical identification of the transmissivity coefficient in the one-dimensi...
For two-dimensional groundwater flow in an isotropic confined aquifer, it has been shown elsewhere t...
The mass balance equation for stationary flow in a confined aquifer and the phenomenological Darcy s...
We identify simultaneously the hydraulic transmissivity and the storage coefficient in a ground wate...
We identify simultaneously the hydraulic transmissivity and the storage coefficient in a ground wate...
The paper is devoted to the inverse problem of identifying the coefficient in the main term of a qua...
The identification of the transmissivity, T, of a confined aquifer, for which the 2D flow condition ...
The paper deals with the identification of unknown storativity and transmissiv-ity distributions wit...
International audienceThe paper deals with the identification of unknown storativity and transmissiv...
The Authors suggest an approximate approch for the solution of the problem of the identification of ...
The Authors suggest an approximate approch for the solution of the problem of the identification of ...
The Authors suggest an approximate approch for the solution of the problem of the identification of ...
This paper is devoted to the inverse problem of identifying a spatially varying coefficient in a lin...
The differential system (DS) method for the identification of transmissivity and storativity is appl...
This paper is devoted to the inverse problem of identifying a spatially varying coefficient in a lin...
AbstractWe discuss the numerical identification of the transmissivity coefficient in the one-dimensi...
For two-dimensional groundwater flow in an isotropic confined aquifer, it has been shown elsewhere t...
The mass balance equation for stationary flow in a confined aquifer and the phenomenological Darcy s...
We identify simultaneously the hydraulic transmissivity and the storage coefficient in a ground wate...
We identify simultaneously the hydraulic transmissivity and the storage coefficient in a ground wate...
The paper is devoted to the inverse problem of identifying the coefficient in the main term of a qua...
The identification of the transmissivity, T, of a confined aquifer, for which the 2D flow condition ...
The paper deals with the identification of unknown storativity and transmissiv-ity distributions wit...
International audienceThe paper deals with the identification of unknown storativity and transmissiv...