| Titre de série : |
Geological survey water - supply paper, 2046 |
| Titre : |
Calibration of a mathematical model of the Antelope valley groundwater basin, California |
| Type de document : |
texte imprimé |
| Auteurs : |
Durbin, T. J. |
| Mention d'édition : |
U.S. government Printing Office |
| Editeur : |
U.S. Government Printing Office |
| Année de publication : |
1978 |
| ISBN/ISSN/EAN : |
CI03B708 |
| Note générale : |
Antelope valley is a closed topographic basin in the western part of the mopve desert in southern California. A groundwater basin with a surface area of 900 square miles (2.300 square kilometers) and a thickness of as much as 5,000 feet (1,500 meters) underlies the valley floor. The groundwater system consists of two alluvial aquifers separated by fine - grained lacustrine deposit. During the last 50 years, pumpage of groundwater is excess of naturel recharge has resqulted in the steady deline of the groundwater level in basin. To help evaluate the possible impact of various water management alternatives, a mathematical model of thez groundwater basin was constructed. |
| Langues : |
Anglais (eng) |
| Mots-clés : |
PUITS Eau souterraine Modèle mathématique Alimentation en eau Hydrologie Cartologie |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
Antelope valley is a closed topographic basin in the western part of the mopve desert in southern California. A groundwater basin with a surface area of 900 square miles (2.300 square kilometers) and a thickness of as much as 5,000 feet (1,500 meters) underlies the valley floor. The groundwater system consists of two alluvial aquifers separated by fine - grained lacustrine deposit. During the last 50 years, pumpage of groundwater is excess of naturel recharge has resqulted in the steady deline of the groundwater level in basin. To help evaluate the possible impact of various water management alternatives, a mathematical model of thez groundwater basin was constructed. |
| Note de contenu : |
Antelope valley is a closed topographic basin in the western part of the mopve desert in southern California. A groundwater basin with a surface area of 900 square miles (2.300 square kilometers) and a thickness of as much as 5,000 feet (1,500 meters) underlies the valley floor. The groundwater system consists of two alluvial aquifers separated by fine - grained lacustrine deposit. During the last 50 years, pumpage of groundwater is excess of naturel recharge has resqulted in the steady deline of the groundwater level in basin. To help evaluate the possible impact of various water management alternatives, a mathematical model of thez groundwater basin was constructed. |
Geological survey water - supply paper, 2046. Calibration of a mathematical model of the Antelope valley groundwater basin, California [texte imprimé] / Durbin, T. J. . - U.S. government Printing Office . - U.S. Government Printing Office, 1978. ISSN : CI03B708 Antelope valley is a closed topographic basin in the western part of the mopve desert in southern California. A groundwater basin with a surface area of 900 square miles (2.300 square kilometers) and a thickness of as much as 5,000 feet (1,500 meters) underlies the valley floor. The groundwater system consists of two alluvial aquifers separated by fine - grained lacustrine deposit. During the last 50 years, pumpage of groundwater is excess of naturel recharge has resqulted in the steady deline of the groundwater level in basin. To help evaluate the possible impact of various water management alternatives, a mathematical model of thez groundwater basin was constructed. Langues : Anglais ( eng)
| Mots-clés : |
PUITS Eau souterraine Modèle mathématique Alimentation en eau Hydrologie Cartologie |
| Index. décimale : |
551.48 Hydrologie : |
| Résumé : |
Antelope valley is a closed topographic basin in the western part of the mopve desert in southern California. A groundwater basin with a surface area of 900 square miles (2.300 square kilometers) and a thickness of as much as 5,000 feet (1,500 meters) underlies the valley floor. The groundwater system consists of two alluvial aquifers separated by fine - grained lacustrine deposit. During the last 50 years, pumpage of groundwater is excess of naturel recharge has resqulted in the steady deline of the groundwater level in basin. To help evaluate the possible impact of various water management alternatives, a mathematical model of thez groundwater basin was constructed. |
| Note de contenu : |
Antelope valley is a closed topographic basin in the western part of the mopve desert in southern California. A groundwater basin with a surface area of 900 square miles (2.300 square kilometers) and a thickness of as much as 5,000 feet (1,500 meters) underlies the valley floor. The groundwater system consists of two alluvial aquifers separated by fine - grained lacustrine deposit. During the last 50 years, pumpage of groundwater is excess of naturel recharge has resqulted in the steady deline of the groundwater level in basin. To help evaluate the possible impact of various water management alternatives, a mathematical model of thez groundwater basin was constructed. |
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