| Titre de série : |
Geological survey water-nepply paper, 2039-B |
| Titre : |
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 : |
United States Government Printing Office |
| Editeur : |
United States Government Printing Office |
| Année de publication : |
1976 |
| ISBN/ISSN/EAN : |
CI-04869 |
| Note générale : |
Supplemental irrigation of well-drained sandy soils has prompted an evaluation of ground water in the appleton area. Glacial duft aquifers are the largest source of ground water. The surficial outwash most areally extensive drift aquifer, and it underlies much of the randy soil area- Saturated thichness of the outwash is more than 80 feet (24m) in places, and potential well yields may exceed 1,200 gal/min (76 1/s) in some areas. In about 17 percent of the area, yield of more than 300 gal (19 1/s) are obtainable. |
| Langues : |
Anglais (eng) |
| Mots-clés : |
Eau souterraine Irrigation Géologie Qualité de l'eau Eau de surface Hydraulique villageoise Modèle mathématique |
| 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 duft aquifers are the largest source of ground water. The surficial outwash most areally extensive drift aquifer, and it underlies much of the randy soil area- Saturated thichness of the outwash is more than 80 feet (24m) in places, and potential well yields may exceed 1,200 gal/min (76 1/s) in some areas. In about 17 percent of the area, yield of more than 300 gal (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 duft aquifers are the largest source of ground water. The surficial outwash most areally extensive drift aquifer, and it underlies much of the randy soil area- Saturated thichness of the outwash is more than 80 feet (24m) in places, and potential well yields may exceed 1,200 gal/min (76 1/s) in some areas. In about 17 percent of the area, yield of more than 300 gal (19 1/s) are obtainable. |
Geological survey water-nepply paper, 2039-B. An appraisal of ground water for irrigation in the appleton area, west-central Minnesota [texte imprimé] / Larson, S. P. . - United States Government Printing Office . - United States Government Printing Office, 1976. ISSN : CI-04869 Supplemental irrigation of well-drained sandy soils has prompted an evaluation of ground water in the appleton area. Glacial duft aquifers are the largest source of ground water. The surficial outwash most areally extensive drift aquifer, and it underlies much of the randy soil area- Saturated thichness of the outwash is more than 80 feet (24m) in places, and potential well yields may exceed 1,200 gal/min (76 1/s) in some areas. In about 17 percent of the area, yield of more than 300 gal (19 1/s) are obtainable. Langues : Anglais ( eng)
| Mots-clés : |
Eau souterraine Irrigation Géologie Qualité de l'eau Eau de surface Hydraulique villageoise Modèle mathématique |
| 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 duft aquifers are the largest source of ground water. The surficial outwash most areally extensive drift aquifer, and it underlies much of the randy soil area- Saturated thichness of the outwash is more than 80 feet (24m) in places, and potential well yields may exceed 1,200 gal/min (76 1/s) in some areas. In about 17 percent of the area, yield of more than 300 gal (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 duft aquifers are the largest source of ground water. The surficial outwash most areally extensive drift aquifer, and it underlies much of the randy soil area- Saturated thichness of the outwash is more than 80 feet (24m) in places, and potential well yields may exceed 1,200 gal/min (76 1/s) in some areas. In about 17 percent of the area, yield of more than 300 gal (19 1/s) are obtainable. |
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