Titre de série :	U.S. Geological Survey Water Supply paper, n°2380
Titre :	Geochemical relations and distribution of selected trace elements in ground water of the northern port of the western : San Joaquim valley, California
Type de document :	texte imprimé
Auteurs :	Dubrovsky, N. M. ; Neil, J. M. ; Welker, M. C.
Mention d'édition :	U.S. Department of the interior
Editeur :	U.S. Department of the Interior
Année de publication :	1991
ISBN/ISSN/EAN :	CI-07607
Note générale :	Water samptes were collected from 44 wells in the northern part of the western San Joaquim Valley, California, between march and july 1985 to assess the geochemical relations and distribution of major ions and selected trace element concentrations in groundwater of the area. The ground water -flow system consists of a semiconfined zone and a confined zone separted by a regoinally extensive clay bed. The data shows that the area and vertical distribution of ground water chemidry in the groundwater-flow system has been affected by different agricultural and national sources of recharge and the source and redox statuts of the sediments...
Langues :	Anglais (eng)
Mots-clés :	Eau  Eau souterraine  Geochimie  Hydrogéologie
Index. décimale :	551.48 Hydrologie :
Résumé :	Water samptes were collected from 44 wells in the northern part of the western San Joaquim Valley, California, between march and july 1985 to assess the geochemical relations and distribution of major ions and selected trace element concentrations in groundwater of the area. The ground water -flow system consists of a semiconfined zone and a confined zone separted by a regoinally extensive clay bed. The data shows that the area and vertical distribution of ground water chemidry in the groundwater-flow system has been affected by different agricultural and national sources of recharge and the source and redox statuts of the sediments...
Note de contenu :	Water samptes were collected from 44 wells in the northern part of the western San Joaquim Valley, California, between march and july 1985 to assess the geochemical relations and distribution of major ions and selected trace element concentrations in groundwater of the area. The ground water -flow system consists of a semiconfined zone and a confined zone separted by a regoinally extensive clay bed. The data shows that the area and vertical distribution of ground water chemidry in the groundwater-flow system has been affected by different agricultural and national sources of recharge and the source and redox statuts of the sediments...

U.S. Geological Survey Water Supply paper, n°2380. Geochemical relations and distribution of selected trace elements in ground water of the northern port of the western : San Joaquim valley, California [texte imprimé] / Dubrovsky, N. M. ; Neil, J. M. ; Welker, M. C.  . -  U.S. Department of the interior . - U.S. Department of the Interior, 1991.
ISSN : CI-07607
Water samptes were collected from 44 wells in the northern part of the western San Joaquim Valley, California, between march and july 1985 to assess the geochemical relations and distribution of major ions and selected trace element concentrations in groundwater of the area. The ground water -flow system consists of a semiconfined zone and a confined zone separted by a regoinally extensive clay bed. The data shows that the area and vertical distribution of ground water chemidry in the groundwater-flow system has been affected by different agricultural and national sources of recharge and the source and redox statuts of the sediments...
Langues : Anglais (eng)

Mots-clés :	Eau  Eau souterraine  Geochimie  Hydrogéologie
Index. décimale :	551.48 Hydrologie :
Résumé :	Water samptes were collected from 44 wells in the northern part of the western San Joaquim Valley, California, between march and july 1985 to assess the geochemical relations and distribution of major ions and selected trace element concentrations in groundwater of the area. The ground water -flow system consists of a semiconfined zone and a confined zone separted by a regoinally extensive clay bed. The data shows that the area and vertical distribution of ground water chemidry in the groundwater-flow system has been affected by different agricultural and national sources of recharge and the source and redox statuts of the sediments...
Note de contenu :	Water samptes were collected from 44 wells in the northern part of the western San Joaquim Valley, California, between march and july 1985 to assess the geochemical relations and distribution of major ions and selected trace element concentrations in groundwater of the area. The ground water -flow system consists of a semiconfined zone and a confined zone separted by a regoinally extensive clay bed. The data shows that the area and vertical distribution of ground water chemidry in the groundwater-flow system has been affected by different agricultural and national sources of recharge and the source and redox statuts of the sediments...