U.S. Geological survey-water paper, 2341-B. Evaluations of site -selection criteria, well design, monitoring technic, and cost analysis for a ground-water supply in piedmont crystalline kocks, North Carolina / Daniel, C.

Public ISBD Titre de série : U.S. Geological survey-water paper, 2341-B Titre : Evaluations of site -selection criteria, well design, monitoring technic, and cost analysis for a ground-water supply in piedmont crystalline kocks, North Carolina Type de document : texte imprimé Auteurs : Daniel, C. Mention d'édition : U.S. Geological survey, Federal center Editeur : U.S. Geological Survey, Federal Center Année de publication : 1990 ISBN/ISSN/EAN : CI-06007 Note générale : A statistical analysis of data from wells drilled into the crystalline rocks of the piedmont and the ridge provinces of north Carolina verified and refined previously proposed criteria for the siting of wells to describes major aspects of ground-water supply development in piedmont crystalline rocks. These aspects are (1) evaluation of well site-selection criteria (2) well -construction design, (3) technic for monotoring well performance, and (4) analysis of cost. This report describes the cary ground-water development program from its begining in early 1981. Langues : Anglais (eng) Mots-clés : Evaluation  Eau souterraine  Hydrogéologie  Roche cristalline Index. décimale : 551.48 Hydrologie : Résumé : A statistical analysis of data from wells drilled into the crystalline rocks of the piedmont and the ridge provinces of north Carolina verified and refined previously proposed criteria for the siting of wells to describes major aspects of ground-water supply development in piedmont crystalline rocks. These aspects are (1) evaluation of well site-selection criteria (2) well -construction design, (3) technic for monotoring well performance, and (4) analysis of cost. This report describes the cary ground-water development program from its begining in early 1981. Note de contenu : A statistical analysis of data from wells drilled into the crystalline rocks of the piedmont and the ridge provinces of north Carolina verified and refined previously proposed criteria for the siting of wells to describes major aspects of ground-water supply development in piedmont crystalline rocks. These aspects are (1) evaluation of well site-selection criteria (2) well -construction design, (3) technic for monotoring well performance, and (4) analysis of cost. This report describes the cary ground-water development program from its begining in early 1981. U.S. Geological survey-water paper, 2341-B. Evaluations of site -selection criteria, well design, monitoring technic, and cost analysis for a ground-water supply in piedmont crystalline kocks, North Carolina [texte imprimé] / Daniel, C.  . -  U.S. Geological survey, Federal center . - U.S. Geological Survey, Federal Center, 1990. ISSN : CI-06007 A statistical analysis of data from wells drilled into the crystalline rocks of the piedmont and the ridge provinces of north Carolina verified and refined previously proposed criteria for the siting of wells to describes major aspects of ground-water supply development in piedmont crystalline rocks. These aspects are (1) evaluation of well site-selection criteria (2) well -construction design, (3) technic for monotoring well performance, and (4) analysis of cost. This report describes the cary ground-water development program from its begining in early 1981. Langues : Anglais (eng) Mots-clés : Evaluation  Eau souterraine  Hydrogéologie  Roche cristalline Index. décimale : 551.48 Hydrologie : Résumé : A statistical analysis of data from wells drilled into the crystalline rocks of the piedmont and the ridge provinces of north Carolina verified and refined previously proposed criteria for the siting of wells to describes major aspects of ground-water supply development in piedmont crystalline rocks. These aspects are (1) evaluation of well site-selection criteria (2) well -construction design, (3) technic for monotoring well performance, and (4) analysis of cost. This report describes the cary ground-water development program from its begining in early 1981. Note de contenu : A statistical analysis of data from wells drilled into the crystalline rocks of the piedmont and the ridge provinces of north Carolina verified and refined previously proposed criteria for the siting of wells to describes major aspects of ground-water supply development in piedmont crystalline rocks. These aspects are (1) evaluation of well site-selection criteria (2) well -construction design, (3) technic for monotoring well performance, and (4) analysis of cost. This report describes the cary ground-water development program from its begining in early 1981.

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U. S. Geological Survey Water Supply paper, 2280. Magnitude and frequency of high flows of unregulated streams in Kansas / Jordan, P. R.

Public ISBD Titre de série : U. S. Geological Survey Water Supply paper, 2280 Titre : Magnitude and frequency of high flows of unregulated streams in Kansas Type de document : texte imprimé Auteurs : Jordan, P. R. Mention d'édition : U.S. Geological Survey, Federal Center Editeur : U.S. Geological Survey, Federal Center Année de publication : 1986 ISBN/ISSN/EAN : CI-05043 Note générale : Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... Langues : Anglais (eng) Mots-clés : Eau de surface  Ruissellement  Inondation  Barrage  Mesure et observation  Prévention  Sécurité des barrages Index. décimale : 627.8 Barrages Résumé : Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... Note de contenu : Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... U. S. Geological Survey Water Supply paper, 2280. Magnitude and frequency of high flows of unregulated streams in Kansas [texte imprimé] / Jordan, P. R.  . -  U.S. Geological Survey, Federal Center . - U.S. Geological Survey, Federal Center, 1986. ISSN : CI-05043 Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... Langues : Anglais (eng) Mots-clés : Eau de surface  Ruissellement  Inondation  Barrage  Mesure et observation  Prévention  Sécurité des barrages Index. décimale : 627.8 Barrages Résumé : Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... Note de contenu : Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated...

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U.S . Geological survey water-supply paper, 2321. Using geophysical logs to estimate porosity, water resistinty, and intrinc permeability / Jorgensen, D. G.

Public ISBD Titre de série : U.S . Geological survey water-supply paper, 2321 Titre : Using geophysical logs to estimate porosity, water resistinty, and intrinc permeability Type de document : texte imprimé Auteurs : Jorgensen, D. G. Mention d'édition : U.S. Geological survey, Federal Center Editeur : U.S. Geological Survey, Federal Center Année de publication : 1989 ISBN/ISSN/EAN : CI-06009 Note générale : Geophysical logs can be to estimate porosity, formation-water resistivity, and intrinsic permeability for geohydrologic investigations, especially in areas where measurements of these geohydrology properties are not available. This paper is to describe selected technic of unsing borehole-geophysical logs for each technic the assumptions upon which it is based, and measured data for comparison and evaluation are presented for each technic. Then this paper is directed to hydrologists investigating water resources in aquifers for wich hydraulic data are sparse, such as most deeply buried rock sections and assumes a cursory knowledge of geophysical logging. Langues : Anglais (eng) Mots-clés : Géophysique  Eau  Perméabilité du sol  Hydrologie Index. décimale : 551.48 Hydrologie : Résumé : Geophysical logs can be to estimate porosity, formation-water resistivity, and intrinsic permeability for geohydrologic investigations, especially in areas where measurements of these geohydrology properties are not available. This paper is to describe selected technic of unsing borehole-geophysical logs for each technic the assumptions upon which it is based, and measured data for comparison and evaluation are presented for each technic. Then this paper is directed to hydrologists investigating water resources in aquifers for wich hydraulic data are sparse, such as most deeply buried rock sections and assumes a cursory knowledge of geophysical logging. Note de contenu : Geophysical logs can be to estimate porosity, formation-water resistivity, and intrinsic permeability for geohydrologic investigations, especially in areas where measurements of these geohydrology properties are not available. This paper is to describe selected technic of unsing borehole-geophysical logs for each technic the assumptions upon which it is based, and measured data for comparison and evaluation are presented for each technic. Then this paper is directed to hydrologists investigating water resources in aquifers for wich hydraulic data are sparse, such as most deeply buried rock sections and assumes a cursory knowledge of geophysical logging. U.S . Geological survey water-supply paper, 2321. Using geophysical logs to estimate porosity, water resistinty, and intrinc permeability [texte imprimé] / Jorgensen, D. G.  . -  U.S. Geological survey, Federal Center . - U.S. Geological Survey, Federal Center, 1989. ISSN : CI-06009 Geophysical logs can be to estimate porosity, formation-water resistivity, and intrinsic permeability for geohydrologic investigations, especially in areas where measurements of these geohydrology properties are not available. This paper is to describe selected technic of unsing borehole-geophysical logs for each technic the assumptions upon which it is based, and measured data for comparison and evaluation are presented for each technic. Then this paper is directed to hydrologists investigating water resources in aquifers for wich hydraulic data are sparse, such as most deeply buried rock sections and assumes a cursory knowledge of geophysical logging. Langues : Anglais (eng) Mots-clés : Géophysique  Eau  Perméabilité du sol  Hydrologie Index. décimale : 551.48 Hydrologie : Résumé : Geophysical logs can be to estimate porosity, formation-water resistivity, and intrinsic permeability for geohydrologic investigations, especially in areas where measurements of these geohydrology properties are not available. This paper is to describe selected technic of unsing borehole-geophysical logs for each technic the assumptions upon which it is based, and measured data for comparison and evaluation are presented for each technic. Then this paper is directed to hydrologists investigating water resources in aquifers for wich hydraulic data are sparse, such as most deeply buried rock sections and assumes a cursory knowledge of geophysical logging. Note de contenu : Geophysical logs can be to estimate porosity, formation-water resistivity, and intrinsic permeability for geohydrologic investigations, especially in areas where measurements of these geohydrology properties are not available. This paper is to describe selected technic of unsing borehole-geophysical logs for each technic the assumptions upon which it is based, and measured data for comparison and evaluation are presented for each technic. Then this paper is directed to hydrologists investigating water resources in aquifers for wich hydraulic data are sparse, such as most deeply buried rock sections and assumes a cursory knowledge of geophysical logging.

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U.S. Geological Survey Water Supply paper, 2327. Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in north-western Illinois / Healy, R. W.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2327 Titre : Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in north-western Illinois Type de document : texte imprimé Auteurs : Healy, R. W. ; Vries, M. P. de ; Sturrock, A. M. Mention d'édition : U.S. Geological Survey, Federal Center Editeur : U.S. Geological Survey, Federal Center Année de publication : 1989 ISBN/ISSN/EAN : CI-05046 Note générale : From July 1982 though june 1987, a study was made of the evapotranspiration and microclimate at a low-level radioactive disposal site near sheffield, Bureau, County, Illinois. This report presents the theory methods, and results of a 2-year study of evapotranspiration and microclimate conducted at the low-level radioactive waste disposal site near sheffield, Illinois. Included is a description of the microclimate and estimates of evapotranspiration at the site for the period of data collection. Details on the microclimate are provided so that assumption inherent in each method used to estimate evapotranspiration may be fully undertood. Three different methods were used to estimate evapotranspiration : energy budget/Bowen ratio, aerodynamic profile, and water budget... Langues : Anglais (eng) Mots-clés : PRECIPITATIONS  Evaporation  Climatologie  Météorologie  Sol  Végétation  Energie  Evapotranspiration Index. décimale : 551.6 Climatologie et temps Résumé : From July 1982 though june 1987, a study was made of the evapotranspiration and microclimate at a low-level radioactive disposal site near sheffield, Bureau, County, Illinois. This report presents the theory methods, and results of a 2-year study of evapotranspiration and microclimate conducted at the low-level radioactive waste disposal site near sheffield, Illinois. Included is a description of the microclimate and estimates of evapotranspiration at the site for the period of data collection. Details on the microclimate are provided so that assumption inherent in each method used to estimate evapotranspiration may be fully undertood. Three different methods were used to estimate evapotranspiration : energy budget/Bowen ratio, aerodynamic profile, and water budget... Note de contenu : From July 1982 though june 1987, a study was made of the evapotranspiration and microclimate at a low-level radioactive disposal site near sheffield, Bureau, County, Illinois. This report presents the theory methods, and results of a 2-year study of evapotranspiration and microclimate conducted at the low-level radioactive waste disposal site near sheffield, Illinois. Included is a description of the microclimate and estimates of evapotranspiration at the site for the period of data collection. Details on the microclimate are provided so that assumption inherent in each method used to estimate evapotranspiration may be fully undertood. Three different methods were used to estimate evapotranspiration : energy budget/Bowen ratio, aerodynamic profile, and water budget... U.S. Geological Survey Water Supply paper, 2327. Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in north-western Illinois [texte imprimé] / Healy, R. W. ; Vries, M. P. de ; Sturrock, A. M.  . -  U.S. Geological Survey, Federal Center . - U.S. Geological Survey, Federal Center, 1989. ISSN : CI-05046 From July 1982 though june 1987, a study was made of the evapotranspiration and microclimate at a low-level radioactive disposal site near sheffield, Bureau, County, Illinois. This report presents the theory methods, and results of a 2-year study of evapotranspiration and microclimate conducted at the low-level radioactive waste disposal site near sheffield, Illinois. Included is a description of the microclimate and estimates of evapotranspiration at the site for the period of data collection. Details on the microclimate are provided so that assumption inherent in each method used to estimate evapotranspiration may be fully undertood. Three different methods were used to estimate evapotranspiration : energy budget/Bowen ratio, aerodynamic profile, and water budget... Langues : Anglais (eng) Mots-clés : PRECIPITATIONS  Evaporation  Climatologie  Météorologie  Sol  Végétation  Energie  Evapotranspiration Index. décimale : 551.6 Climatologie et temps Résumé : From July 1982 though june 1987, a study was made of the evapotranspiration and microclimate at a low-level radioactive disposal site near sheffield, Bureau, County, Illinois. This report presents the theory methods, and results of a 2-year study of evapotranspiration and microclimate conducted at the low-level radioactive waste disposal site near sheffield, Illinois. Included is a description of the microclimate and estimates of evapotranspiration at the site for the period of data collection. Details on the microclimate are provided so that assumption inherent in each method used to estimate evapotranspiration may be fully undertood. Three different methods were used to estimate evapotranspiration : energy budget/Bowen ratio, aerodynamic profile, and water budget... Note de contenu : From July 1982 though june 1987, a study was made of the evapotranspiration and microclimate at a low-level radioactive disposal site near sheffield, Bureau, County, Illinois. This report presents the theory methods, and results of a 2-year study of evapotranspiration and microclimate conducted at the low-level radioactive waste disposal site near sheffield, Illinois. Included is a description of the microclimate and estimates of evapotranspiration at the site for the period of data collection. Details on the microclimate are provided so that assumption inherent in each method used to estimate evapotranspiration may be fully undertood. Three different methods were used to estimate evapotranspiration : energy budget/Bowen ratio, aerodynamic profile, and water budget...

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U.S. Geological survey -water supply paper, 2332. Hydrologic characteristic of the great salt lake, utach : 1847-1960 / Arnow, T.

Public ISBD Titre de série : U.S. Geological survey -water supply paper, 2332 Titre : Hydrologic characteristic of the great salt lake, utach : 1847-1960 Type de document : texte imprimé Auteurs : Arnow, T. ; Stephens, D. Mention d'édition : U.S. Geological survey, Federal center Editeur : U.S. Geological Survey, Federal Center Année de publication : 1990 ISBN/ISSN/EAN : CI-06006 Note générale : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. Langues : Anglais (eng) Mots-clés : Hydrologie  Eau souterraine  PRECIPITATIONS  Débit solide Index. décimale : 551.48 Hydrologie : Résumé : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. Note de contenu : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. U.S. Geological survey -water supply paper, 2332. Hydrologic characteristic of the great salt lake, utach : 1847-1960 [texte imprimé] / Arnow, T. ; Stephens, D.  . -  U.S. Geological survey, Federal center . - U.S. Geological Survey, Federal Center, 1990. ISSN : CI-06006 The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. Langues : Anglais (eng) Mots-clés : Hydrologie  Eau souterraine  PRECIPITATIONS  Débit solide Index. décimale : 551.48 Hydrologie : Résumé : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish. Note de contenu : The great salt lake in Utah is a large of water bordered on the west by barren desert and on the east by a major metropolitan area. It is the fourth largest terminal lake in the world covering about 2, 300 square miles in 1986. Since its histoire low elevation of 4, 191.35 feet in 1986. Most of this increase (12.2 feet) occured after 1982. The rise has caused 285 millions of damage to lake side industries transportation farming, and wildlife. Accompagnying the rapid rise in lake level has been a decrease in salinity -from 28 percent in 1963 to about 6 percent in 1986. This resuted in changes in the bista of the lake from obligate haclophiles to opportupistic form such as blue-green and, most recently, a brackish fish.

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U.S. Geological survey water -supply paper, 2343. Evaluation of nonpotable ground water in the desert area of southeastern California for powerplant cooling / Steineman, A. C.

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U.S. Geological survey water-supply paper, 2347. Urban stormwater runoff selected background information and technics for problem assessment, with a baltimord, Maryland, case study / Fisher, G. T.

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U.S. Geological survey water-supply paper, 2368. Description of the physical environment and coal -mining history of west - central indiana with emphasis on six small watersheds / Martin, J. D.

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U-S. Geological Survey Water-Supply Paper. Estimates of evapotranspiration in alkaline scrub and meadow communities of Ovens valley, California, using the Bowen-Ratio, Eddy-correlation, and Penman-Combination methods / Duell, L. F. W.

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US geological Survey Water Supply Paper, 2297. Estimation of recharge rates to the sand and gravel aquifer using environmental tritium, Nantucket Island, Massachusetts / Knott, F. F.

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