Titre de série :	Water Ressource
Titre :	Modeling of mass transport in a carbonate aquifer
Type de document :	texte imprimé
Auteurs :	Rybnikova, L. S. ; Lekhov, A. V.
Année de publication :	1986
ISBN/ISSN/EAN :	CI-11686
Note générale :	The model mass transport in a carbonate aquifer it is required to develop special method taking into account the characteristics of the structure of the bed. Carbonate rocks represent heterogeneous systems for which markedly different flow and storage properties of the permeable channels. (Fractures) and poorly permeable porous blocks are characteristic. A mathematical description by the method of schematization of the filtering meduim. The equations of mass transport in a heterogeneous system are also usually written differentially for the fracture and block and are interrelated by the rate of mass exhange . This article examines a migration scheme and combined numerical and analytical method of modeling the profile two dimensional transport of a contaminate in a carbonate aquifer from a source located on the surface.
Langues :	Anglais (eng)
Mots-clés :	Modélisation  Débit solide  Perméabilité du sol  Roche  Modèle mathématique  Bassin hydrogéologique
Index. décimale :	551 Géologie, météorologie, hydrologie générale
Résumé :	The model mass transport in a carbonate aquifer it is required to develop special method taking into account the characteristics of the structure of the bed. Carbonate rocks represent heterogeneous systems for which markedly different flow and storage properties of the permeable channels. (Fractures) and poorly permeable porous blocks are characteristic. A mathematical description by the method of schematization of the filtering meduim. The equations of mass transport in a heterogeneous system are also usually written differentially for the fracture and block and are interrelated by the rate of mass exhange . This article examines a migration scheme and combined numerical and analytical method of modeling the profile two dimensional transport of a contaminate in a carbonate aquifer from a source located on the surface.
Note de contenu :	The model mass transport in a carbonate aquifer it is required to develop special method taking into account the characteristics of the structure of the bed. Carbonate rocks represent heterogeneous systems for which markedly different flow and storage properties of the permeable channels. (Fractures) and poorly permeable porous blocks are characteristic. A mathematical description by the method of schematization of the filtering meduim. The equations of mass transport in a heterogeneous system are also usually written differentially for the fracture and block and are interrelated by the rate of mass exhange . This article examines a migration scheme and combined numerical and analytical method of modeling the profile two dimensional transport of a contaminate in a carbonate aquifer from a source located on the surface.

Water Ressource. Modeling of mass transport in a carbonate aquifer [texte imprimé] / Rybnikova, L. S. ; Lekhov, A. V. . - 1986.
ISSN : CI-11686
The model mass transport in a carbonate aquifer it is required to develop special method taking into account the characteristics of the structure of the bed. Carbonate rocks represent heterogeneous systems for which markedly different flow and storage properties of the permeable channels. (Fractures) and poorly permeable porous blocks are characteristic. A mathematical description by the method of schematization of the filtering meduim. The equations of mass transport in a heterogeneous system are also usually written differentially for the fracture and block and are interrelated by the rate of mass exhange . This article examines a migration scheme and combined numerical and analytical method of modeling the profile two dimensional transport of a contaminate in a carbonate aquifer from a source located on the surface.
Langues : Anglais (eng)

Mots-clés :	Modélisation  Débit solide  Perméabilité du sol  Roche  Modèle mathématique  Bassin hydrogéologique
Index. décimale :	551 Géologie, météorologie, hydrologie générale
Résumé :	The model mass transport in a carbonate aquifer it is required to develop special method taking into account the characteristics of the structure of the bed. Carbonate rocks represent heterogeneous systems for which markedly different flow and storage properties of the permeable channels. (Fractures) and poorly permeable porous blocks are characteristic. A mathematical description by the method of schematization of the filtering meduim. The equations of mass transport in a heterogeneous system are also usually written differentially for the fracture and block and are interrelated by the rate of mass exhange . This article examines a migration scheme and combined numerical and analytical method of modeling the profile two dimensional transport of a contaminate in a carbonate aquifer from a source located on the surface.
Note de contenu :	The model mass transport in a carbonate aquifer it is required to develop special method taking into account the characteristics of the structure of the bed. Carbonate rocks represent heterogeneous systems for which markedly different flow and storage properties of the permeable channels. (Fractures) and poorly permeable porous blocks are characteristic. A mathematical description by the method of schematization of the filtering meduim. The equations of mass transport in a heterogeneous system are also usually written differentially for the fracture and block and are interrelated by the rate of mass exhange . This article examines a migration scheme and combined numerical and analytical method of modeling the profile two dimensional transport of a contaminate in a carbonate aquifer from a source located on the surface.