U.S. Geological Survey Water Supply paper, 2208. Streamflow augmentation at fosters brook, Long island, New York - A hydraulic feasability study / Prince, K. R.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2208 Titre : Streamflow augmentation at fosters brook, Long island, New York - A hydraulic feasability study Type de document : texte imprimé Auteurs : Prince, K. R. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1984 ISBN/ISSN/EAN : CI-05071 Note générale : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. Langues : Anglais (eng) Mots-clés : Eau de surface  Eau souterraine  Infiltration  Hydrochimie  Température de l'eau  Modèle numérique Index. décimale : 551.48 Hydrologie : Résumé : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. Note de contenu : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. U.S. Geological Survey Water Supply paper, 2208. Streamflow augmentation at fosters brook, Long island, New York - A hydraulic feasability study [texte imprimé] / Prince, K. R.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1984. ISSN : CI-05071 A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. Langues : Anglais (eng) Mots-clés : Eau de surface  Eau souterraine  Infiltration  Hydrochimie  Température de l'eau  Modèle numérique Index. décimale : 551.48 Hydrologie : Résumé : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. Note de contenu : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours.

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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 / Prince, K. R.

Public ISBD 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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