| 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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