Titre :	Mathematical models for hydrolic process
Type de document :	texte imprimé
Auteurs :	Marsily, G. (de)
Année de publication :	1972
ISBN/ISSN/EAN :	CI-06638
Note générale :	Models of simulation of ground flow in sedimentary basins are generally used for water resources optimization problems / however, a by product to their building way be additional information on the structure of the basins themselves. In the first stage of the simulation procedure, the hydraulic parameters of the sediments (permeability, porosity) have to be determined, using lithostratigraphical and hydrologic data. The values of these parameters are closed related to the sedimentation process itself. Two different techniques of identification of these parameters are presented Practival examples on tertiary marine sediments in aquitaine, and quaternary alluvial sediments, will show the complement of information gained in this manner of the structure of the basins.
Langues :	Anglais (eng)
Mots-clés :	Hydrologie  Modèle mathématique  Simulation  Eau souterraine  Sédimentation  Géologie  Méthodologie  Acquifère  Equation  Paramètre hydraulique
Index. décimale :	551.48 Hydrologie :
Résumé :	Models of simulation of ground flow in sedimentary basins are generally used for water resources optimization problems / however, a by product to their building way be additional information on the structure of the basins themselves. In the first stage of the simulation procedure, the hydraulic parameters of the sediments (permeability, porosity) have to be determined, using lithostratigraphical and hydrologic data. The values of these parameters are closed related to the sedimentation process itself. Two different techniques of identification of these parameters are presented Practival examples on tertiary marine sediments in aquitaine, and quaternary alluvial sediments, will show the complement of information gained in this manner of the structure of the basins.
Note de contenu :	Models of simulation of ground flow in sedimentary basins are generally used for water resources optimization problems / however, a by product to their building way be additional information on the structure of the basins themselves. In the first stage of the simulation procedure, the hydraulic parameters of the sediments (permeability, porosity) have to be determined, using lithostratigraphical and hydrologic data. The values of these parameters are closed related to the sedimentation process itself. Two different techniques of identification of these parameters are presented Practival examples on tertiary marine sediments in aquitaine, and quaternary alluvial sediments, will show the complement of information gained in this manner of the structure of the basins.

Mathematical models for hydrolic process [texte imprimé] / Marsily, G. (de) . - 1972.
ISSN : CI-06638
Models of simulation of ground flow in sedimentary basins are generally used for water resources optimization problems / however, a by product to their building way be additional information on the structure of the basins themselves. In the first stage of the simulation procedure, the hydraulic parameters of the sediments (permeability, porosity) have to be determined, using lithostratigraphical and hydrologic data. The values of these parameters are closed related to the sedimentation process itself. Two different techniques of identification of these parameters are presented Practival examples on tertiary marine sediments in aquitaine, and quaternary alluvial sediments, will show the complement of information gained in this manner of the structure of the basins.
Langues : Anglais (eng)

Mots-clés :	Hydrologie  Modèle mathématique  Simulation  Eau souterraine  Sédimentation  Géologie  Méthodologie  Acquifère  Equation  Paramètre hydraulique
Index. décimale :	551.48 Hydrologie :
Résumé :	Models of simulation of ground flow in sedimentary basins are generally used for water resources optimization problems / however, a by product to their building way be additional information on the structure of the basins themselves. In the first stage of the simulation procedure, the hydraulic parameters of the sediments (permeability, porosity) have to be determined, using lithostratigraphical and hydrologic data. The values of these parameters are closed related to the sedimentation process itself. Two different techniques of identification of these parameters are presented Practival examples on tertiary marine sediments in aquitaine, and quaternary alluvial sediments, will show the complement of information gained in this manner of the structure of the basins.
Note de contenu :	Models of simulation of ground flow in sedimentary basins are generally used for water resources optimization problems / however, a by product to their building way be additional information on the structure of the basins themselves. In the first stage of the simulation procedure, the hydraulic parameters of the sediments (permeability, porosity) have to be determined, using lithostratigraphical and hydrologic data. The values of these parameters are closed related to the sedimentation process itself. Two different techniques of identification of these parameters are presented Practival examples on tertiary marine sediments in aquitaine, and quaternary alluvial sediments, will show the complement of information gained in this manner of the structure of the basins.