U.S. Geological Survey Water Supplu paper, 2209. Digital models of ground-water flow in the Cape cod aquifer system, Massachusetts / Gusuva, J. H.

Public ISBD Titre de série : U.S. Geological Survey Water Supplu paper, 2209 Titre : Digital models of ground-water flow in the Cape cod aquifer system, Massachusetts Type de document : texte imprimé Auteurs : Gusuva, J. H. ; Leblanc, D. R. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1985 ISBN/ISSN/EAN : CI-05070 Note générale : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d Langues : Anglais (eng) Mots-clés : Eau souterraine  Bassin versant  Eau salée  Eau douce  Ruissellement  Simulation  Evaluation Index. décimale : 551.49 Eaux souterraines Résumé : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d Note de contenu : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d U.S. Geological Survey Water Supplu paper, 2209. Digital models of ground-water flow in the Cape cod aquifer system, Massachusetts [texte imprimé] / Gusuva, J. H. ; Leblanc, D. R.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1985. ISSN : CI-05070 The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d Langues : Anglais (eng) Mots-clés : Eau souterraine  Bassin versant  Eau salée  Eau douce  Ruissellement  Simulation  Evaluation Index. décimale : 551.49 Eaux souterraines Résumé : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d Note de contenu : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d

Réservation

Réserver ce document

Exemplaires(8)

Code-barres	Cote	Support	Localisation	Section	Disponibilité
CI03B070.77746	CI-05070	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B070.77745	CI-05070	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B070.77744	CI-05070	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B070.77743	CI-05070	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B070.77742	CI-05070	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B070.77741	CI-05070	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B070.77740	CI-05070	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
CI03B070.77739	CI-05070	Monographie	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible

---

1 (1 - 1 / 1) Par page : 25 50 100 200