Titre de série : |
U.S. Geological Survey Water Supply paper, 2309 |
Titre : |
Quantitative assessment of the shallow ground-water flow system associated with Connetquot Brook, Long Island, New York |
Type de document : |
texte imprimé |
Auteurs : |
Prince, K. R. ; Franke, L. O. ; Reilly, T. E. |
Mention d'édition : |
United States Gouvernement Printing Office |
Editeur : |
United States Gouvernement Printing Office |
Année de publication : |
1988 |
ISBN/ISSN/EAN : |
CI-05081 |
Note générale : |
Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. |
Langues : |
Anglais (eng) |
Mots-clés : |
Eau souterraine Bassin versant Drainage Hydrochimie Mesure et observation Météorologie Simulation Evaluation quantitative |
Index. décimale : |
551.48 Hydrologie : |
Résumé : |
Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. |
Note de contenu : |
Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. |
U.S. Geological Survey Water Supply paper, 2309. Quantitative assessment of the shallow ground-water flow system associated with Connetquot Brook, Long Island, New York [texte imprimé] / Prince, K. R. ; Franke, L. O. ; Reilly, T. E. . - United States Gouvernement Printing Office . - United States Gouvernement Printing Office, 1988. ISSN : CI-05081 Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. Langues : Anglais ( eng)
Mots-clés : |
Eau souterraine Bassin versant Drainage Hydrochimie Mesure et observation Météorologie Simulation Evaluation quantitative |
Index. décimale : |
551.48 Hydrologie : |
Résumé : |
Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. |
Note de contenu : |
Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. |
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