Titre de série :	Geological survey water supply paper, 2039-B
Titre :	Contribution to the hydrology of the United States : an appraisal of ground water for irrigation in the appleton area, West Central Minnesota
Type de document :	texte imprimé
Auteurs :	Larson, S. P.
Mention d'édition :	US Government printing office
Editeur :	US Government Printing Office
Année de publication :	1976
ISBN/ISSN/EAN :	CI-08237
Note générale :	Supplemental irrigation of well drained sandy soils has prompted an evaluation of ground water in the appleton area. Glacial drift aquifers are the largest source of ground water. The surficial outwash sand and gravel is the most readily available and the most areally extensive drift aquifer, and it underlines much of the sandy oil area. Saturated thickness of the outwash is more than 80 feet (24 m) in places, and potential well yield may exceed 1,200 qal/min (76 1/s) in some areas. In about 17 percent of the area, yields of more than 300 qal / min (19 1/s) are obtainable.
Langues :	Français (fre)
Mots-clés :	Eau souterraine  Irrigation  Hydrologie  Géologie  Qualité de l'eau  Bassin HYDROGEOLOGIE
Index. décimale :	631.58 Méthodes de culture : jachère, assolement irrigation
Résumé :	Supplemental irrigation of well drained sandy soils has prompted an evaluation of ground water in the appleton area. Glacial drift aquifers are the largest source of ground water. The surficial outwash sand and gravel is the most readily available and the most areally extensive drift aquifer, and it underlines much of the sandy oil area. Saturated thickness of the outwash is more than 80 feet (24 m) in places, and potential well yield may exceed 1,200 qal/min (76 1/s) in some areas. In about 17 percent of the area, yields of more than 300 qal / min (19 1/s) are obtainable.
Note de contenu :	Supplemental irrigation of well drained sandy soils has prompted an evaluation of ground water in the appleton area. Glacial drift aquifers are the largest source of ground water. The surficial outwash sand and gravel is the most readily available and the most areally extensive drift aquifer, and it underlines much of the sandy oil area. Saturated thickness of the outwash is more than 80 feet (24 m) in places, and potential well yield may exceed 1,200 qal/min (76 1/s) in some areas. In about 17 percent of the area, yields of more than 300 qal / min (19 1/s) are obtainable.

Geological survey water supply paper, 2039-B. Contribution to the hydrology of the United States : an appraisal of ground water for irrigation in the appleton area, West Central Minnesota [texte imprimé] / Larson, S. P.  . -  US Government printing office . - US Government Printing Office, 1976.
ISSN : CI-08237
Supplemental irrigation of well drained sandy soils has prompted an evaluation of ground water in the appleton area. Glacial drift aquifers are the largest source of ground water. The surficial outwash sand and gravel is the most readily available and the most areally extensive drift aquifer, and it underlines much of the sandy oil area. Saturated thickness of the outwash is more than 80 feet (24 m) in places, and potential well yield may exceed 1,200 qal/min (76 1/s) in some areas. In about 17 percent of the area, yields of more than 300 qal / min (19 1/s) are obtainable.
Langues : Français (fre)

Mots-clés :	Eau souterraine  Irrigation  Hydrologie  Géologie  Qualité de l'eau  Bassin HYDROGEOLOGIE
Index. décimale :	631.58 Méthodes de culture : jachère, assolement irrigation
Résumé :	Supplemental irrigation of well drained sandy soils has prompted an evaluation of ground water in the appleton area. Glacial drift aquifers are the largest source of ground water. The surficial outwash sand and gravel is the most readily available and the most areally extensive drift aquifer, and it underlines much of the sandy oil area. Saturated thickness of the outwash is more than 80 feet (24 m) in places, and potential well yield may exceed 1,200 qal/min (76 1/s) in some areas. In about 17 percent of the area, yields of more than 300 qal / min (19 1/s) are obtainable.
Note de contenu :	Supplemental irrigation of well drained sandy soils has prompted an evaluation of ground water in the appleton area. Glacial drift aquifers are the largest source of ground water. The surficial outwash sand and gravel is the most readily available and the most areally extensive drift aquifer, and it underlines much of the sandy oil area. Saturated thickness of the outwash is more than 80 feet (24 m) in places, and potential well yield may exceed 1,200 qal/min (76 1/s) in some areas. In about 17 percent of the area, yields of more than 300 qal / min (19 1/s) are obtainable.