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.