U.S. Geological Survey Water Supply paper, 2353. Geohydrology and model analysis of stream-aquifer system along the Arkansas river in Kearny an Finney countries, Southwestern Kansas / Dunlap, L. E.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2353 Titre : Geohydrology and model analysis of stream-aquifer system along the Arkansas river in Kearny an Finney countries, Southwestern Kansas Type de document : texte imprimé Auteurs : Dunlap, L. E. ; Lindgren, R. J. ; Sauer, C. G. Mention d'édition : U. S. Geological Survey Editeur : U. S. Geological Survey Année de publication : 1985 ISBN/ISSN/EAN : CI-05095 Note générale : A study was made in cooperation with the division of Water Resources, Kansas State Board of agriculture to determine geohydrolgie conditons in an area comprising nearly 850,000 acres along the Arkansas River valley in Kearny and Finney countries, southwestern Kansas. This report describes the geohydrology of Kearny and Finney courntries along the Arkansas River, studied under phase II, and a computer-model analysis of the associated stream-aquifer system. The report is written for the scientically informed public and for state and local water agencies who may use the results of the investigations to formulate water management policies to improve the conjunctive use of ground and surface water within the constraints of the water rights structure in Kansas. Langues : Anglais (eng) Mots-clés : Hydrogéologie  Bassin versant  Eau souterraine  Eau de surface  Hydrologie  Modelisation  Simulation Index. décimale : 551.48 Hydrologie : Résumé : A study was made in cooperation with the division of Water Resources, Kansas State Board of agriculture to determine geohydrolgie conditons in an area comprising nearly 850,000 acres along the Arkansas River valley in Kearny and Finney countries, southwestern Kansas. This report describes the geohydrology of Kearny and Finney courntries along the Arkansas River, studied under phase II, and a computer-model analysis of the associated stream-aquifer system. The report is written for the scientically informed public and for state and local water agencies who may use the results of the investigations to formulate water management policies to improve the conjunctive use of ground and surface water within the constraints of the water rights structure in Kansas. Note de contenu : A study was made in cooperation with the division of Water Resources, Kansas State Board of agriculture to determine geohydrolgie conditons in an area comprising nearly 850,000 acres along the Arkansas River valley in Kearny and Finney countries, southwestern Kansas. This report describes the geohydrology of Kearny and Finney courntries along the Arkansas River, studied under phase II, and a computer-model analysis of the associated stream-aquifer system. The report is written for the scientically informed public and for state and local water agencies who may use the results of the investigations to formulate water management policies to improve the conjunctive use of ground and surface water within the constraints of the water rights structure in Kansas. U.S. Geological Survey Water Supply paper, 2353. Geohydrology and model analysis of stream-aquifer system along the Arkansas river in Kearny an Finney countries, Southwestern Kansas [texte imprimé] / Dunlap, L. E. ; Lindgren, R. J. ; Sauer, C. G.  . -  U. S. Geological Survey . - U. S. Geological Survey, 1985. ISSN : CI-05095 A study was made in cooperation with the division of Water Resources, Kansas State Board of agriculture to determine geohydrolgie conditons in an area comprising nearly 850,000 acres along the Arkansas River valley in Kearny and Finney countries, southwestern Kansas. This report describes the geohydrology of Kearny and Finney courntries along the Arkansas River, studied under phase II, and a computer-model analysis of the associated stream-aquifer system. The report is written for the scientically informed public and for state and local water agencies who may use the results of the investigations to formulate water management policies to improve the conjunctive use of ground and surface water within the constraints of the water rights structure in Kansas. Langues : Anglais (eng) Mots-clés : Hydrogéologie  Bassin versant  Eau souterraine  Eau de surface  Hydrologie  Modelisation  Simulation Index. décimale : 551.48 Hydrologie : Résumé : A study was made in cooperation with the division of Water Resources, Kansas State Board of agriculture to determine geohydrolgie conditons in an area comprising nearly 850,000 acres along the Arkansas River valley in Kearny and Finney countries, southwestern Kansas. This report describes the geohydrology of Kearny and Finney courntries along the Arkansas River, studied under phase II, and a computer-model analysis of the associated stream-aquifer system. The report is written for the scientically informed public and for state and local water agencies who may use the results of the investigations to formulate water management policies to improve the conjunctive use of ground and surface water within the constraints of the water rights structure in Kansas. Note de contenu : A study was made in cooperation with the division of Water Resources, Kansas State Board of agriculture to determine geohydrolgie conditons in an area comprising nearly 850,000 acres along the Arkansas River valley in Kearny and Finney countries, southwestern Kansas. This report describes the geohydrology of Kearny and Finney courntries along the Arkansas River, studied under phase II, and a computer-model analysis of the associated stream-aquifer system. The report is written for the scientically informed public and for state and local water agencies who may use the results of the investigations to formulate water management policies to improve the conjunctive use of ground and surface water within the constraints of the water rights structure in Kansas.

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U.S. Geological Survey Water Supply paper, 2355. Water quality essessment of the delmarva peninsula, Delaware, maryland, and Virginia - Analysis of available Ground - water - quality data through 1987 / Hamilton, P.A.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2355 Titre : Water quality essessment of the delmarva peninsula, Delaware, maryland, and Virginia - Analysis of available Ground - water - quality data through 1987 Type de document : texte imprimé Auteurs : Hamilton, P.A. ; Shedlock, R. J. ; Philips, P. J. Mention d'édition : U.S. Department of the Interior Editeur : U.S. Department of the Interior Année de publication : 1991 ISBN/ISSN/EAN : CI-08233 Note générale : 1 Langues : Anglais (eng) Mots-clés : Qualité de l'eau  Eau souterraine  Distribution Index. décimale : 551.49 Eaux souterraines Résumé : 1 Note de contenu : 1 U.S. Geological Survey Water Supply paper, 2355. Water quality essessment of the delmarva peninsula, Delaware, maryland, and Virginia - Analysis of available Ground - water - quality data through 1987 [texte imprimé] / Hamilton, P.A. ; Shedlock, R. J. ; Philips, P. J.  . -  U.S. Department of the Interior . - U.S. Department of the Interior, 1991. ISSN : CI-08233 1 Langues : Anglais (eng) Mots-clés : Qualité de l'eau  Eau souterraine  Distribution Index. décimale : 551.49 Eaux souterraines Résumé : 1 Note de contenu : 1

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U.S. Geological Survey Water Supply paper, 2370. Etimation soil matric potential in owens valley, California / Sorenson, S. K.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2370 Titre : Etimation soil matric potential in owens valley, California Type de document : texte imprimé Auteurs : Sorenson, S. K. ; Miller, R. F. ; Welch, M. R. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1989 ISBN/ISSN/EAN : CI-05062 Note générale : Evaluation of the modeling technique at two study sites indicated that estimates of soil matric potential within 0,5 per units of the soil matric potential value derived by using the filter-paper method could be obtained 90 to 95 percent of the time in soils where water content was less than field capacity. The greatest errors occured at depths where there was a distinct transition between soils of different textures. Langues : Anglais (eng) Mots-clés : Eau souterraine  Sol  Evaluation  Modèle mathématique  Méthode d'évaluation Index. décimale : 551.49 Eaux souterraines Résumé : Evaluation of the modeling technique at two study sites indicated that estimates of soil matric potential within 0,5 per units of the soil matric potential value derived by using the filter-paper method could be obtained 90 to 95 percent of the time in soils where water content was less than field capacity. The greatest errors occured at depths where there was a distinct transition between soils of different textures. Note de contenu : Evaluation of the modeling technique at two study sites indicated that estimates of soil matric potential within 0,5 per units of the soil matric potential value derived by using the filter-paper method could be obtained 90 to 95 percent of the time in soils where water content was less than field capacity. The greatest errors occured at depths where there was a distinct transition between soils of different textures. U.S. Geological Survey Water Supply paper, 2370. Etimation soil matric potential in owens valley, California [texte imprimé] / Sorenson, S. K. ; Miller, R. F. ; Welch, M. R.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1989. ISSN : CI-05062 Evaluation of the modeling technique at two study sites indicated that estimates of soil matric potential within 0,5 per units of the soil matric potential value derived by using the filter-paper method could be obtained 90 to 95 percent of the time in soils where water content was less than field capacity. The greatest errors occured at depths where there was a distinct transition between soils of different textures. Langues : Anglais (eng) Mots-clés : Eau souterraine  Sol  Evaluation  Modèle mathématique  Méthode d'évaluation Index. décimale : 551.49 Eaux souterraines Résumé : Evaluation of the modeling technique at two study sites indicated that estimates of soil matric potential within 0,5 per units of the soil matric potential value derived by using the filter-paper method could be obtained 90 to 95 percent of the time in soils where water content was less than field capacity. The greatest errors occured at depths where there was a distinct transition between soils of different textures. Note de contenu : Evaluation of the modeling technique at two study sites indicated that estimates of soil matric potential within 0,5 per units of the soil matric potential value derived by using the filter-paper method could be obtained 90 to 95 percent of the time in soils where water content was less than field capacity. The greatest errors occured at depths where there was a distinct transition between soils of different textures.

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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 / Dubrovsky, N. M.

Public ISBD 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...

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