U.S. Gealogical Survey Water Supply paper, 2210. Connector well experiment to recharge theFloridan aquifer, East Orange county, Florida / Bush, P. W.

Public ISBD Titre de série : U.S. Gealogical Survey Water Supply paper, 2210 Titre : Connector well experiment to recharge theFloridan aquifer, East Orange county, Florida Type de document : texte imprimé Auteurs : Bush, P. W. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1983 ISBN/ISSN/EAN : CI-05072 Note générale : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrologie  Hydrogéologie  Eau souterraine  PUITS  Expérimentation Index. décimale : 551.48 Hydrologie : Résumé : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. Note de contenu : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. U.S. Gealogical Survey Water Supply paper, 2210. Connector well experiment to recharge theFloridan aquifer, East Orange county, Florida [texte imprimé] / Bush, P. W.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1983. ISSN : CI-05072 An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrologie  Hydrogéologie  Eau souterraine  PUITS  Expérimentation Index. décimale : 551.48 Hydrologie : Résumé : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers. Note de contenu : An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in East orange county, Flo., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer/ hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well connecting the two aquifers.

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U.S. Geological Survey Water paper, 2244. Cost-effectiveness of the stream gaging program in maine a prototype for nationwide implementation / Fontaine, R. A.

Public ISBD Titre de série : U.S. Geological Survey Water paper, 2244 Titre : Cost-effectiveness of the stream gaging program in maine a prototype for nationwide implementation Type de document : texte imprimé Auteurs : Fontaine, R. A. ; Moss, M. E. ; Smath, J. A. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1984 ISBN/ISSN/EAN : CI-05088 Note générale : This report documents the results of a cost-effectiveness study of the stream-gaging program in Maine. Data uses and funding sources were identified for the 51 coninuous stream gages currently being operated in Maine with a budget of $ 211,000. Three stream gages were identified as producting data no longer sufficiently needed to warrant continuing their operation. Operation of these stations should be discontinued. Data collected at three other stations were identified as having uses specific only to short-term studies/ it is recommended that these stations be discontinued at the end of the data-colletion phases of the studies.The remaining 45 stations should be maintained in the program for the foreseable future. Langues : Anglais (eng) Mots-clés : Ruissellement  Qualité de l'eau  Mesure et observation  Modèle mathématique Index. décimale : 553.7 Eau : classer ici les ouvrages généraux sur l'eau Résumé : This report documents the results of a cost-effectiveness study of the stream-gaging program in Maine. Data uses and funding sources were identified for the 51 coninuous stream gages currently being operated in Maine with a budget of $ 211,000. Three stream gages were identified as producting data no longer sufficiently needed to warrant continuing their operation. Operation of these stations should be discontinued. Data collected at three other stations were identified as having uses specific only to short-term studies/ it is recommended that these stations be discontinued at the end of the data-colletion phases of the studies.The remaining 45 stations should be maintained in the program for the foreseable future. Note de contenu : This report documents the results of a cost-effectiveness study of the stream-gaging program in Maine. Data uses and funding sources were identified for the 51 coninuous stream gages currently being operated in Maine with a budget of $ 211,000. Three stream gages were identified as producting data no longer sufficiently needed to warrant continuing their operation. Operation of these stations should be discontinued. Data collected at three other stations were identified as having uses specific only to short-term studies/ it is recommended that these stations be discontinued at the end of the data-colletion phases of the studies.The remaining 45 stations should be maintained in the program for the foreseable future. U.S. Geological Survey Water paper, 2244. Cost-effectiveness of the stream gaging program in maine a prototype for nationwide implementation [texte imprimé] / Fontaine, R. A. ; Moss, M. E. ; Smath, J. A.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1984. ISSN : CI-05088 This report documents the results of a cost-effectiveness study of the stream-gaging program in Maine. Data uses and funding sources were identified for the 51 coninuous stream gages currently being operated in Maine with a budget of $ 211,000. Three stream gages were identified as producting data no longer sufficiently needed to warrant continuing their operation. Operation of these stations should be discontinued. Data collected at three other stations were identified as having uses specific only to short-term studies/ it is recommended that these stations be discontinued at the end of the data-colletion phases of the studies.The remaining 45 stations should be maintained in the program for the foreseable future. Langues : Anglais (eng) Mots-clés : Ruissellement  Qualité de l'eau  Mesure et observation  Modèle mathématique Index. décimale : 553.7 Eau : classer ici les ouvrages généraux sur l'eau Résumé : This report documents the results of a cost-effectiveness study of the stream-gaging program in Maine. Data uses and funding sources were identified for the 51 coninuous stream gages currently being operated in Maine with a budget of $ 211,000. Three stream gages were identified as producting data no longer sufficiently needed to warrant continuing their operation. Operation of these stations should be discontinued. Data collected at three other stations were identified as having uses specific only to short-term studies/ it is recommended that these stations be discontinued at the end of the data-colletion phases of the studies.The remaining 45 stations should be maintained in the program for the foreseable future. Note de contenu : This report documents the results of a cost-effectiveness study of the stream-gaging program in Maine. Data uses and funding sources were identified for the 51 coninuous stream gages currently being operated in Maine with a budget of $ 211,000. Three stream gages were identified as producting data no longer sufficiently needed to warrant continuing their operation. Operation of these stations should be discontinued. Data collected at three other stations were identified as having uses specific only to short-term studies/ it is recommended that these stations be discontinued at the end of the data-colletion phases of the studies.The remaining 45 stations should be maintained in the program for the foreseable future.

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U.S. Geological Survey Water Supplu paper, 2185 - F. Water quality of north Carolina streams - water quality characteristicc for selected sites on the cape fear river, North Caraolina, 1955 - 80 variability, loads, and trends of selct contituents / Crawford, J. K.

Public ISBD Titre de série : U.S. Geological Survey Water Supplu paper, 2185 - F Titre : Water quality of north Carolina streams - water quality characteristicc for selected sites on the cape fear river, North Caraolina, 1955 - 80 variability, loads, and trends of selct contituents Type de document : texte imprimé Auteurs : Crawford, J. K. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1985 ISBN/ISSN/EAN : CI-05112 Note générale : Capter A of this report describes in detail the initial design and philosophy of the U S. Geological Survey Water quality programm in North Carolina. Specific methodologies for the estimation of baseline water quality, pollution and the evaluation of strends in water quality discussed in chapter A are applied and the refined in subsequient chapters that present water quality assessments of individual large rivers. Chapter B elaborates on the methodology used in estimating baseline survey. Chapters C and D present water quality assessments of the French Board and Neuse Rivers, respectively. Chapter E is a water quality assessment of the Yadkin-Pee Dee River system. Chapter F assesses water quality in the cape Fear river and concludes the series. Langues : Anglais (eng) Mots-clés : Pollution  Qualité de l'eau  Climat  Géologie  Population  Hydrologie  Temperature  Hydrogéologie Index. décimale : 551.48 Hydrologie : Résumé : Capter A of this report describes in detail the initial design and philosophy of the U S. Geological Survey Water quality programm in North Carolina. Specific methodologies for the estimation of baseline water quality, pollution and the evaluation of strends in water quality discussed in chapter A are applied and the refined in subsequient chapters that present water quality assessments of individual large rivers. Chapter B elaborates on the methodology used in estimating baseline survey. Chapters C and D present water quality assessments of the French Board and Neuse Rivers, respectively. Chapter E is a water quality assessment of the Yadkin-Pee Dee River system. Chapter F assesses water quality in the cape Fear river and concludes the series. Note de contenu : Capter A of this report describes in detail the initial design and philosophy of the U S. Geological Survey Water quality programm in North Carolina. Specific methodologies for the estimation of baseline water quality, pollution and the evaluation of strends in water quality discussed in chapter A are applied and the refined in subsequient chapters that present water quality assessments of individual large rivers. Chapter B elaborates on the methodology used in estimating baseline survey. Chapters C and D present water quality assessments of the French Board and Neuse Rivers, respectively. Chapter E is a water quality assessment of the Yadkin-Pee Dee River system. Chapter F assesses water quality in the cape Fear river and concludes the series. U.S. Geological Survey Water Supplu paper, 2185 - F. Water quality of north Carolina streams - water quality characteristicc for selected sites on the cape fear river, North Caraolina, 1955 - 80 variability, loads, and trends of selct contituents [texte imprimé] / Crawford, J. K.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1985. ISSN : CI-05112 Capter A of this report describes in detail the initial design and philosophy of the U S. Geological Survey Water quality programm in North Carolina. Specific methodologies for the estimation of baseline water quality, pollution and the evaluation of strends in water quality discussed in chapter A are applied and the refined in subsequient chapters that present water quality assessments of individual large rivers. Chapter B elaborates on the methodology used in estimating baseline survey. Chapters C and D present water quality assessments of the French Board and Neuse Rivers, respectively. Chapter E is a water quality assessment of the Yadkin-Pee Dee River system. Chapter F assesses water quality in the cape Fear river and concludes the series. Langues : Anglais (eng) Mots-clés : Pollution  Qualité de l'eau  Climat  Géologie  Population  Hydrologie  Temperature  Hydrogéologie Index. décimale : 551.48 Hydrologie : Résumé : Capter A of this report describes in detail the initial design and philosophy of the U S. Geological Survey Water quality programm in North Carolina. Specific methodologies for the estimation of baseline water quality, pollution and the evaluation of strends in water quality discussed in chapter A are applied and the refined in subsequient chapters that present water quality assessments of individual large rivers. Chapter B elaborates on the methodology used in estimating baseline survey. Chapters C and D present water quality assessments of the French Board and Neuse Rivers, respectively. Chapter E is a water quality assessment of the Yadkin-Pee Dee River system. Chapter F assesses water quality in the cape Fear river and concludes the series. Note de contenu : Capter A of this report describes in detail the initial design and philosophy of the U S. Geological Survey Water quality programm in North Carolina. Specific methodologies for the estimation of baseline water quality, pollution and the evaluation of strends in water quality discussed in chapter A are applied and the refined in subsequient chapters that present water quality assessments of individual large rivers. Chapter B elaborates on the methodology used in estimating baseline survey. Chapters C and D present water quality assessments of the French Board and Neuse Rivers, respectively. Chapter E is a water quality assessment of the Yadkin-Pee Dee River system. Chapter F assesses water quality in the cape Fear river and concludes the series.

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U.S. Geological Survey Water Supplu paper, 2209. Digital models of ground-water flow in the Cape cod aquifer system, Massachusetts / Gusuva, J. H.

Public ISBD Titre de série : U.S. Geological Survey Water Supplu paper, 2209 Titre : Digital models of ground-water flow in the Cape cod aquifer system, Massachusetts Type de document : texte imprimé Auteurs : Gusuva, J. H. ; Leblanc, D. R. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1985 ISBN/ISSN/EAN : CI-05070 Note générale : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d Langues : Anglais (eng) Mots-clés : Eau souterraine  Bassin versant  Eau salée  Eau douce  Ruissellement  Simulation  Evaluation Index. décimale : 551.49 Eaux souterraines Résumé : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d Note de contenu : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d U.S. Geological Survey Water Supplu paper, 2209. Digital models of ground-water flow in the Cape cod aquifer system, Massachusetts [texte imprimé] / Gusuva, J. H. ; Leblanc, D. R.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1985. ISSN : CI-05070 The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d Langues : Anglais (eng) Mots-clés : Eau souterraine  Bassin versant  Eau salée  Eau douce  Ruissellement  Simulation  Evaluation Index. décimale : 551.49 Eaux souterraines Résumé : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d Note de contenu : The Cape cod aquifer system was simulated with three dimensional dinite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal. The model boundaries were selected to represent the natural hydrologic boundaries af the aquifer. The boundary between fresh and saline ground water was treated as an interface along which there is no dispersion. Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and groundwater was treated as static. d

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U.S. Geological Survey Water Supplu paper, 2212. Water quality in the new river from calexico to the salton sea imperial county, California / Setmire, J.G.

Public ISBD Titre de série : U.S. Geological Survey Water Supplu paper, 2212 Titre : Water quality in the new river from calexico to the salton sea imperial county, California Type de document : texte imprimé Auteurs : Setmire, J.G. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1984 ISBN/ISSN/EAN : CI-05074 Note générale : The New River enters the United States at Calexico, Californie, after it crosses the international boundary. Water-quality data from routine collection indicated that the new river was degraded by high organic and bacterial content. Intensive sampling for chemical and physical constituents and properties of the river was done may 9 - 13, 1977, to quantify the chemical composition of the water and to identify water-quality problems. Concentrations of total organic carbon in the New River at Calexico renged from 80 to 161 milligrams per liter and dissolved organic carbon ranged from 34 to 42 milligrams per liter. Intensive sampling for chemical and biological characteristics was done in the New River from may 1977 to june 1978 to determine the occurence of the organic material ans its effects on downstream water quality. Langues : Anglais (eng) Mots-clés : Hydrologie  Eau de surface  Qualité de l'eau  Matière organique  Hydrochimie Index. décimale : 551.48 Hydrologie : Résumé : The New River enters the United States at Calexico, Californie, after it crosses the international boundary. Water-quality data from routine collection indicated that the new river was degraded by high organic and bacterial content. Intensive sampling for chemical and physical constituents and properties of the river was done may 9 - 13, 1977, to quantify the chemical composition of the water and to identify water-quality problems. Concentrations of total organic carbon in the New River at Calexico renged from 80 to 161 milligrams per liter and dissolved organic carbon ranged from 34 to 42 milligrams per liter. Intensive sampling for chemical and biological characteristics was done in the New River from may 1977 to june 1978 to determine the occurence of the organic material ans its effects on downstream water quality. Note de contenu : The New River enters the United States at Calexico, Californie, after it crosses the international boundary. Water-quality data from routine collection indicated that the new river was degraded by high organic and bacterial content. Intensive sampling for chemical and physical constituents and properties of the river was done may 9 - 13, 1977, to quantify the chemical composition of the water and to identify water-quality problems. Concentrations of total organic carbon in the New River at Calexico renged from 80 to 161 milligrams per liter and dissolved organic carbon ranged from 34 to 42 milligrams per liter. Intensive sampling for chemical and biological characteristics was done in the New River from may 1977 to june 1978 to determine the occurence of the organic material ans its effects on downstream water quality. U.S. Geological Survey Water Supplu paper, 2212. Water quality in the new river from calexico to the salton sea imperial county, California [texte imprimé] / Setmire, J.G.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1984. ISSN : CI-05074 The New River enters the United States at Calexico, Californie, after it crosses the international boundary. Water-quality data from routine collection indicated that the new river was degraded by high organic and bacterial content. Intensive sampling for chemical and physical constituents and properties of the river was done may 9 - 13, 1977, to quantify the chemical composition of the water and to identify water-quality problems. Concentrations of total organic carbon in the New River at Calexico renged from 80 to 161 milligrams per liter and dissolved organic carbon ranged from 34 to 42 milligrams per liter. Intensive sampling for chemical and biological characteristics was done in the New River from may 1977 to june 1978 to determine the occurence of the organic material ans its effects on downstream water quality. Langues : Anglais (eng) Mots-clés : Hydrologie  Eau de surface  Qualité de l'eau  Matière organique  Hydrochimie Index. décimale : 551.48 Hydrologie : Résumé : The New River enters the United States at Calexico, Californie, after it crosses the international boundary. Water-quality data from routine collection indicated that the new river was degraded by high organic and bacterial content. Intensive sampling for chemical and physical constituents and properties of the river was done may 9 - 13, 1977, to quantify the chemical composition of the water and to identify water-quality problems. Concentrations of total organic carbon in the New River at Calexico renged from 80 to 161 milligrams per liter and dissolved organic carbon ranged from 34 to 42 milligrams per liter. Intensive sampling for chemical and biological characteristics was done in the New River from may 1977 to june 1978 to determine the occurence of the organic material ans its effects on downstream water quality. Note de contenu : The New River enters the United States at Calexico, Californie, after it crosses the international boundary. Water-quality data from routine collection indicated that the new river was degraded by high organic and bacterial content. Intensive sampling for chemical and physical constituents and properties of the river was done may 9 - 13, 1977, to quantify the chemical composition of the water and to identify water-quality problems. Concentrations of total organic carbon in the New River at Calexico renged from 80 to 161 milligrams per liter and dissolved organic carbon ranged from 34 to 42 milligrams per liter. Intensive sampling for chemical and biological characteristics was done in the New River from may 1977 to june 1978 to determine the occurence of the organic material ans its effects on downstream water quality.

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U.S. Geological Survey Water Supplu paper, 2228. Evaluation of environmental factors, affecting yields of major disolved ions of streams in the United Sates / Peters, N. E.

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U.S. Geological Survey Water Supply, 2202. Chloroform contamination in part of the alluvial aquifer Southwest Louisville, Kentucky / Davis, R. W.

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U.S. Geological Survey Water Supply aper, 2313. Streamflow, sediment transport, and nutrient transport at incline village, Lake Tahoe, Nevada, 1970 - 73 / Glaney, P. A.

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U.S. Geological Survey Water Supply paper, 2201. Geohydrology and effect of water use in the black mesa area, Navajo and Hopi, Indian reservations, Arizona / Eychaner, J. H.

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U.S. Geological Survey Water Supply paper, 2208. Streamflow augmentation at fosters brook, Long island, New York - A hydraulic feasability study / Prince, K. R.

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U.S. Geological Survey Water Supply paper, 2211. Preliminary evaluation of ground-water contamination by coal-tar derivatives, St. Louis park area, Minnesota / Hult, M.F.

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U.S. Geological Survey Water Supply paper, 2215. Availability and quality of water from the Dakota aquifer, northwest Iowa / Burkart, M. R.

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U.S. Geological Survey Water Supply paper, 2218. Sewage plume in a sand and gravel aquifer, Cape cod, Massachusetts / Le Blanc, D. R.

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U.S. Geological Survey Water Supply paper, 2219. Hydrogeologic setting and the potentiometric surfaces of regional aquifers in the Hollandale embayment, southeastern Minnesota, 1970 - 80 / Delin, G. N.

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U.S. Geological Survey Water Supply paper, 2220. Basic ground-water hydrology / Heath, R. C.

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