U.S. Gealogical Survey Water Supply paper, 2210. Connector well experiment to recharge theFloridan aquifer, East Orange county, Florida / Bush, P. W.

Public ISBD Titre de série : U.S. Gealogical Survey Water Supply paper, 2210 Titre : Connector well experiment to recharge theFloridan aquifer, East Orange county, Florida Type de document : texte imprimé Auteurs : Bush, P. W. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1983 ISBN/ISSN/EAN : CI-05072 Note générale : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrologie  Hydrogéologie  Eau souterraine  PUITS  Expérimentation Index. décimale : 551.48 Hydrologie : Résumé : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. Note de contenu : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. U.S. Gealogical Survey Water Supply paper, 2210. Connector well experiment to recharge theFloridan aquifer, East Orange county, Florida [texte imprimé] / Bush, P. W.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1983. ISSN : CI-05072 An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrologie  Hydrogéologie  Eau souterraine  PUITS  Expérimentation Index. décimale : 551.48 Hydrologie : Résumé : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. Note de contenu : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers.

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U.S. Geological Survey Water Supply paper, 2331. Simulation of saltwater movement in the floridan system, Hilton Head Island, South Carolina / Bush, P. W.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2331 Titre : Simulation of saltwater movement in the floridan system, Hilton Head Island, South Carolina Type de document : texte imprimé Auteurs : Bush, P. W. Mention d'édition : U. S. Geological Survey, Federal Center Editeur : U. S. Geological Survey, Federal Center Année de publication : 1988 ISBN/ISSN/EAN : CI-05048 Note générale : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. Langues : Anglais (eng) Mots-clés : Bassin HYDROGEOLOGIE  Hydrogéologie  Hydrologie  Géologie  Eau souterraine  Eau salée  Eau douce  Simulation Index. décimale : 551.48 Hydrologie : Résumé : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. Note de contenu : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. U.S. Geological Survey Water Supply paper, 2331. Simulation of saltwater movement in the floridan system, Hilton Head Island, South Carolina [texte imprimé] / Bush, P. W.  . -  U. S. Geological Survey, Federal Center . - U. S. Geological Survey, Federal Center, 1988. ISSN : CI-05048 The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. Langues : Anglais (eng) Mots-clés : Bassin HYDROGEOLOGIE  Hydrogéologie  Hydrologie  Géologie  Eau souterraine  Eau salée  Eau douce  Simulation Index. décimale : 551.48 Hydrologie : Résumé : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater. Note de contenu : The seaward hydraulic gradient that existed before pumping begain has been reserved thus increasing the potential for saltwater intrusion. Simulations of predevelopment, recent and future ground water flow in the floridan aquifer system beneath the north end of Hilton Head Island and Port Royal Sound are presented. A finite-element model for fluid-density-dependent ground water flow and solute transport was used in cross section. The general configuration of the simulated predevelopment glowfield is typical of a coastal aquifer having a seaward gradient in the freshwater.

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