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.