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U.S. Geological Survey Water Supplu paper, 2177. Hydrologic effects of stress-relief fracturing in an appallachian valley / Wyrick, G. G.
Titre de série : U.S. Geological Survey Water Supplu paper, 2177 Titre : Hydrologic effects of stress-relief fracturing in an appallachian valley Type de document : texte imprimé Auteurs : Wyrick, G. G. ; Borchers, J. W. Mention d'édition : U. S. Geological Survey Editeur : U. S. Geological Survey Année de publication : 1981 ISBN/ISSN/EAN : CI-05114 Note générale : A hydrologic study at Twin Falls State Park, Wyoming county, West Virginia, was made to determine how fracture systems affect the occurrence and movement of ground water in a typical valley of the Applalachian Plateau Physiographic Province. Twin Falls was selected because it is generally unaffected by factors that would complicate an analysis of the data. The study area was the Black Fork Valley at Twin Falls. The valley is about 3 milles long and 400 to 600 feet wide and is cut into massive sandstone units interbedded with thin coal and shale beds. The study was made to determine how aquifer characteristics were related to fracture systems in this valley, so that the relation could be applied to studies of other valley. Langues : Anglais (eng) Mots-clés : Hydrologie Réseau hydrographique Hydrogéologie Eau souterraine Fracturation Pompage d'essai Index. décimale : 551.48 Hydrologie : Résumé : A hydrologic study at Twin Falls State Park, Wyoming county, West Virginia, was made to determine how fracture systems affect the occurrence and movement of ground water in a typical valley of the Applalachian Plateau Physiographic Province. Twin Falls was selected because it is generally unaffected by factors that would complicate an analysis of the data. The study area was the Black Fork Valley at Twin Falls. The valley is about 3 milles long and 400 to 600 feet wide and is cut into massive sandstone units interbedded with thin coal and shale beds. The study was made to determine how aquifer characteristics were related to fracture systems in this valley, so that the relation could be applied to studies of other valley. Note de contenu : A hydrologic study at Twin Falls State Park, Wyoming county, West Virginia, was made to determine how fracture systems affect the occurrence and movement of ground water in a typical valley of the Applalachian Plateau Physiographic Province. Twin Falls was selected because it is generally unaffected by factors that would complicate an analysis of the data. The study area was the Black Fork Valley at Twin Falls. The valley is about 3 milles long and 400 to 600 feet wide and is cut into massive sandstone units interbedded with thin coal and shale beds. The study was made to determine how aquifer characteristics were related to fracture systems in this valley, so that the relation could be applied to studies of other valley. U.S. Geological Survey Water Supplu paper, 2177. Hydrologic effects of stress-relief fracturing in an appallachian valley [texte imprimé] / Wyrick, G. G. ; Borchers, J. W. . - U. S. Geological Survey . - U. S. Geological Survey, 1981.
ISSN : CI-05114
A hydrologic study at Twin Falls State Park, Wyoming county, West Virginia, was made to determine how fracture systems affect the occurrence and movement of ground water in a typical valley of the Applalachian Plateau Physiographic Province. Twin Falls was selected because it is generally unaffected by factors that would complicate an analysis of the data. The study area was the Black Fork Valley at Twin Falls. The valley is about 3 milles long and 400 to 600 feet wide and is cut into massive sandstone units interbedded with thin coal and shale beds. The study was made to determine how aquifer characteristics were related to fracture systems in this valley, so that the relation could be applied to studies of other valley.
Langues : Anglais (eng)
Mots-clés : Hydrologie Réseau hydrographique Hydrogéologie Eau souterraine Fracturation Pompage d'essai Index. décimale : 551.48 Hydrologie : Résumé : A hydrologic study at Twin Falls State Park, Wyoming county, West Virginia, was made to determine how fracture systems affect the occurrence and movement of ground water in a typical valley of the Applalachian Plateau Physiographic Province. Twin Falls was selected because it is generally unaffected by factors that would complicate an analysis of the data. The study area was the Black Fork Valley at Twin Falls. The valley is about 3 milles long and 400 to 600 feet wide and is cut into massive sandstone units interbedded with thin coal and shale beds. The study was made to determine how aquifer characteristics were related to fracture systems in this valley, so that the relation could be applied to studies of other valley. Note de contenu : A hydrologic study at Twin Falls State Park, Wyoming county, West Virginia, was made to determine how fracture systems affect the occurrence and movement of ground water in a typical valley of the Applalachian Plateau Physiographic Province. Twin Falls was selected because it is generally unaffected by factors that would complicate an analysis of the data. The study area was the Black Fork Valley at Twin Falls. The valley is about 3 milles long and 400 to 600 feet wide and is cut into massive sandstone units interbedded with thin coal and shale beds. The study was made to determine how aquifer characteristics were related to fracture systems in this valley, so that the relation could be applied to studies of other valley. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B114.97265 CI-05114 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B114.97266 CI-05114 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B114.97264 CI-05114 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B114.97263 CI-05114 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B114.97262 CI-05114 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B114.97261 CI-05114 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B114.97260 CI-05114 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B114.97259 CI-05114 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible 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.
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. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B112.77794 CI-05112 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B112.77793 CI-05112 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B112.77792 CI-05112 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B112.77791 CI-05112 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B112.77790 CI-05112 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B112.77789 CI-05112 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B112.77788 CI-05112 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B112.77787 CI-05112 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible 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.
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. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B074.82274 CI-05074 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B074.82273 CI-05074 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B074.82272 CI-05074 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B074.82271 CI-05074 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B074.82270 CI-05074 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B074.82269 CI-05074 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B074.82268 CI-05074 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B074.82267 CI-05074 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U.S. Geological Survey Water Supply, 2202. Chloroform contamination in part of the alluvial aquifer Southwest Louisville, Kentucky / Davis, R. W.
Titre de série : U.S. Geological Survey Water Supply, 2202 Titre : Chloroform contamination in part of the alluvial aquifer Southwest Louisville, Kentucky Type de document : texte imprimé Auteurs : Davis, R. W. ; Matthews, E. W. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1983 ISBN/ISSN/EAN : CI-05103 Note générale : This report presents the two contaminants were above the water table in the alluvium until a long-term trend of rising ground-water levels caused water to reach the contaminants and the water-chloroform mixture began moving dowgradient to the well. The objectives of this study are twofold (1) to determine the source of contamination and the areal extent of ground water contaminated by chloroform and (2) to investigate and evaluate the probable distribution of chloroform in the aquifer under various pumping and nonpumping conditions. Langues : Anglais (eng) Mots-clés : Bassin versant Eau de surface Eau souterraine Hydrogéologie Pollution Chloroforme Carbone Contamination Index. décimale : 551.48 Hydrologie : Résumé : This report presents the two contaminants were above the water table in the alluvium until a long-term trend of rising ground-water levels caused water to reach the contaminants and the water-chloroform mixture began moving dowgradient to the well. The objectives of this study are twofold (1) to determine the source of contamination and the areal extent of ground water contaminated by chloroform and (2) to investigate and evaluate the probable distribution of chloroform in the aquifer under various pumping and nonpumping conditions. Note de contenu : This report presents the two contaminants were above the water table in the alluvium until a long-term trend of rising ground-water levels caused water to reach the contaminants and the water-chloroform mixture began moving dowgradient to the well. The objectives of this study are twofold (1) to determine the source of contamination and the areal extent of ground water contaminated by chloroform and (2) to investigate and evaluate the probable distribution of chloroform in the aquifer under various pumping and nonpumping conditions. U.S. Geological Survey Water Supply, 2202. Chloroform contamination in part of the alluvial aquifer Southwest Louisville, Kentucky [texte imprimé] / Davis, R. W. ; Matthews, E. W. . - United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1983.
ISSN : CI-05103
This report presents the two contaminants were above the water table in the alluvium until a long-term trend of rising ground-water levels caused water to reach the contaminants and the water-chloroform mixture began moving dowgradient to the well. The objectives of this study are twofold (1) to determine the source of contamination and the areal extent of ground water contaminated by chloroform and (2) to investigate and evaluate the probable distribution of chloroform in the aquifer under various pumping and nonpumping conditions.
Langues : Anglais (eng)
Mots-clés : Bassin versant Eau de surface Eau souterraine Hydrogéologie Pollution Chloroforme Carbone Contamination Index. décimale : 551.48 Hydrologie : Résumé : This report presents the two contaminants were above the water table in the alluvium until a long-term trend of rising ground-water levels caused water to reach the contaminants and the water-chloroform mixture began moving dowgradient to the well. The objectives of this study are twofold (1) to determine the source of contamination and the areal extent of ground water contaminated by chloroform and (2) to investigate and evaluate the probable distribution of chloroform in the aquifer under various pumping and nonpumping conditions. Note de contenu : This report presents the two contaminants were above the water table in the alluvium until a long-term trend of rising ground-water levels caused water to reach the contaminants and the water-chloroform mixture began moving dowgradient to the well. The objectives of this study are twofold (1) to determine the source of contamination and the areal extent of ground water contaminated by chloroform and (2) to investigate and evaluate the probable distribution of chloroform in the aquifer under various pumping and nonpumping conditions. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B103.87242 CI-05103 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B103.87241 CI-05103 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B103.87239 CI-05103 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B103.87240 CI-05103 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B103.87238 CI-05103 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B103.87237 CI-05103 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B103.87235 CI-05103 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B103.87236 CI-05103 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U.S. Geological Survey Water Supply, 2205. Mathematical model of the Tesuque aquifer system near Projoaque, New Mexico / Hearne, G. A.
Titre de série : U.S. Geological Survey Water Supply, 2205 Titre : Mathematical model of the Tesuque aquifer system near Projoaque, New Mexico Type de document : texte imprimé Auteurs : Hearne, G. A. Mention d'édition : U. S. Geological Survey Editeur : U. S. Geological Survey Année de publication : 1985 ISBN/ISSN/EAN : CI-05101 Note générale : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. Langues : Anglais (eng) Mots-clés : Bassin versant Eau souterraine Eau de surface Hydrologie Modèle mathématique Bassin hydrologique Index. décimale : 551.48 Hydrologie : Résumé : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. Note de contenu : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. U.S. Geological Survey Water Supply, 2205. Mathematical model of the Tesuque aquifer system near Projoaque, New Mexico [texte imprimé] / Hearne, G. A. . - U. S. Geological Survey . - U. S. Geological Survey, 1985.
ISSN : CI-05101
A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model.
Langues : Anglais (eng)
Mots-clés : Bassin versant Eau souterraine Eau de surface Hydrologie Modèle mathématique Bassin hydrologique Index. décimale : 551.48 Hydrologie : Résumé : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. Note de contenu : A three dimensional digital model ground water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Projoaque river basin and vicinity, New Mexico. The description of the prototype is simple enough to flow a mathematical simulation. This section of the report describes the analogy between the prototype and the model. The description is devided into three subsections : structure aquifer characteristics, and boundaries. In each instance a description of the prototype is followed by a description of the analogy used in the digital model. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B101.77778 CI-05101 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B101.77777 CI-05101 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B101.77776 CI-05101 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B101.77775 CI-05101 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B101.77774 CI-05101 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B101.77773 CI-05101 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B101.77772 CI-05101 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B101.77771 CI-05101 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U.S geological survey water - supply, 2250. National water summary 1983 hydrologic events and Issues
PermalinkU.S. Geological survey water-supply, 2329. Effects of highway runoff on stream flow and water quality in the sevenmile creek basin, a rural area in the piedmont province of north carolina, july 1981 to july 1982 / Harned, D. A.
PermalinkU.S Geological Survey Water-Supply Paper, 1532. Effects of converting sagebrush cover to grass on the hydrology of small watersheds at Boco Mountain, Colorado / Lusby, G.C.
PermalinkU.S Geological Survey Water-Supply Paper, 2057. Hydrology and surface morphology of the Bonneville salt flats and pilot valley Playa, Utah / Lines, G.C.
PermalinkU.S.Geological survey water - supply paper, 2063. Channel and dynamic flow characteristics of the chattahoochee river bufort dam to geogia Highway 141 / Faye, R. E.
PermalinkU.S.Geological Survey Water-supply Paper, 2067. Geochemistry of fluoride in the black creek aquifer system of Horry and Georgetown countries, south Carolina and its physiological implications / Zack, A. L.
PermalinkU.S geological survey water - supply paper, 2079. An annotated Key to the identification of commonly occurring and dominant genera of algae observed in the phytoplankton of the united states / Greeson, P. E.
PermalinkU.S. Geological Survey Water Supply paper, 2176. Chloride in natural continental water : a review / Feth, J. H.
PermalinkU.S. Geological Survey Water Supply paper, 2178. Design of surface water data networks for regional in formation / Moss, M. E.
PermalinkU.S. Geological Survey Water Supply paper, 2179. A statistical analysis of the quality of surface water in Nebraska / Engberg, R. A.
Permalink