U-S. Geological Servey Water-Supply Paper, 2338. Estimation of the recharge area contributing water to a pumped well in a glacialdrift, river-valley aquifer / Morrissey, D. J.

Public ISBD Titre de série : U-S. Geological Servey Water-Supply Paper, 2338 Titre : Estimation of the recharge area contributing water to a pumped well in a glacialdrift, river-valley aquifer Type de document : texte imprimé Auteurs : Morrissey, D. J. Mention d'édition : US Geological Survey, Federal Center Editeur : US geological Survey, Federal Center Année de publication : 1989 ISBN/ISSN/EAN : CI-06637 Note générale : this report describes the factors that affect the size and shape of contributing areas to public supply wells and evaluates several methods that may be used to delineate contributing areas of wells in glacial-drift, river-valley aquifers. Langues : Anglais (eng) Mots-clés : Hydrogéologie  Bassin HYDROGEOLOGIE  Eau  PUITS  Modèle mathématique  Recherche de nappe Index. décimale : 621.2 Hydraulique : turbines, pompes, accumulateurs, transmission hydraulique Résumé : this report describes the factors that affect the size and shape of contributing areas to public supply wells and evaluates several methods that may be used to delineate contributing areas of wells in glacial-drift, river-valley aquifers. Note de contenu : this report describes the factors that affect the size and shape of contributing areas to public supply wells and evaluates several methods that may be used to delineate contributing areas of wells in glacial-drift, river-valley aquifers. U-S. Geological Servey Water-Supply Paper, 2338. Estimation of the recharge area contributing water to a pumped well in a glacialdrift, river-valley aquifer [texte imprimé] / Morrissey, D. J.  . -  US Geological Survey, Federal Center . - US geological Survey, Federal Center, 1989. ISSN : CI-06637 this report describes the factors that affect the size and shape of contributing areas to public supply wells and evaluates several methods that may be used to delineate contributing areas of wells in glacial-drift, river-valley aquifers. Langues : Anglais (eng) Mots-clés : Hydrogéologie  Bassin HYDROGEOLOGIE  Eau  PUITS  Modèle mathématique  Recherche de nappe Index. décimale : 621.2 Hydraulique : turbines, pompes, accumulateurs, transmission hydraulique Résumé : this report describes the factors that affect the size and shape of contributing areas to public supply wells and evaluates several methods that may be used to delineate contributing areas of wells in glacial-drift, river-valley aquifers. Note de contenu : this report describes the factors that affect the size and shape of contributing areas to public supply wells and evaluates several methods that may be used to delineate contributing areas of wells in glacial-drift, river-valley aquifers.

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US geological Survey Water Supply Paper, 2268. Assessment of water ressources in lead-zinc mined areas in Cherokee county, Kansas and adjacent areas / Spruill, T.

Public ISBD Titre de série : US geological Survey Water Supply Paper, 2268 Titre : Assessment of water ressources in lead-zinc mined areas in Cherokee county, Kansas and adjacent areas Type de document : texte imprimé Auteurs : Spruill, T. Mention d'édition : US Geological Survey, Federal Center Editeur : US geological Survey, Federal Center Année de publication : 1987 ISBN/ISSN/EAN : CI-05023 Note générale : "A study was conducted to evaluate water resources problems related to abandoned lead and zinc mines in Cherokee county, Kansas, and adjacent areas in Missouri and Oklahoma. Post mining activities have caused changes in the hydrogeology of the area. Lead and zinc mining has caused discontinuities and perforations in the confining shale west of the Pennsylvania - Mississippian geologic contact which have created artificial ground-water recharge and discharge areas. Recharge to the shallow aquifer through collapses, shafts and drill holes in the shale has caused the formation of a ground-water ""mound"" in the vicinity of the licher field in Kansas and Oklahoma" Langues : Anglais (eng) Mots-clés : Hydrologie  Ressource en eau  Hydrogéologie  Eau de surface  Qualité de l'eau  Evaluation Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : "A study was conducted to evaluate water resources problems related to abandoned lead and zinc mines in Cherokee county, Kansas, and adjacent areas in Missouri and Oklahoma. Post mining activities have caused changes in the hydrogeology of the area. Lead and zinc mining has caused discontinuities and perforations in the confining shale west of the Pennsylvania - Mississippian geologic contact which have created artificial ground-water recharge and discharge areas. Recharge to the shallow aquifer through collapses, shafts and drill holes in the shale has caused the formation of a ground-water ""mound"" in the vicinity of the licher field in Kansas and Oklahoma" Note de contenu : "A study was conducted to evaluate water resources problems related to abandoned lead and zinc mines in Cherokee county, Kansas, and adjacent areas in Missouri and Oklahoma. Post mining activities have caused changes in the hydrogeology of the area. Lead and zinc mining has caused discontinuities and perforations in the confining shale west of the Pennsylvania - Mississippian geologic contact which have created artificial ground-water recharge and discharge areas. Recharge to the shallow aquifer through collapses, shafts and drill holes in the shale has caused the formation of a ground-water ""mound"" in the vicinity of the licher field in Kansas and Oklahoma" US geological Survey Water Supply Paper, 2268. Assessment of water ressources in lead-zinc mined areas in Cherokee county, Kansas and adjacent areas [texte imprimé] / Spruill, T.  . -  US Geological Survey, Federal Center . - US geological Survey, Federal Center, 1987. ISSN : CI-05023 "A study was conducted to evaluate water resources problems related to abandoned lead and zinc mines in Cherokee county, Kansas, and adjacent areas in Missouri and Oklahoma. Post mining activities have caused changes in the hydrogeology of the area. Lead and zinc mining has caused discontinuities and perforations in the confining shale west of the Pennsylvania - Mississippian geologic contact which have created artificial ground-water recharge and discharge areas. Recharge to the shallow aquifer through collapses, shafts and drill holes in the shale has caused the formation of a ground-water ""mound"" in the vicinity of the licher field in Kansas and Oklahoma" Langues : Anglais (eng) Mots-clés : Hydrologie  Ressource en eau  Hydrogéologie  Eau de surface  Qualité de l'eau  Evaluation Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : "A study was conducted to evaluate water resources problems related to abandoned lead and zinc mines in Cherokee county, Kansas, and adjacent areas in Missouri and Oklahoma. Post mining activities have caused changes in the hydrogeology of the area. Lead and zinc mining has caused discontinuities and perforations in the confining shale west of the Pennsylvania - Mississippian geologic contact which have created artificial ground-water recharge and discharge areas. Recharge to the shallow aquifer through collapses, shafts and drill holes in the shale has caused the formation of a ground-water ""mound"" in the vicinity of the licher field in Kansas and Oklahoma" Note de contenu : "A study was conducted to evaluate water resources problems related to abandoned lead and zinc mines in Cherokee county, Kansas, and adjacent areas in Missouri and Oklahoma. Post mining activities have caused changes in the hydrogeology of the area. Lead and zinc mining has caused discontinuities and perforations in the confining shale west of the Pennsylvania - Mississippian geologic contact which have created artificial ground-water recharge and discharge areas. Recharge to the shallow aquifer through collapses, shafts and drill holes in the shale has caused the formation of a ground-water ""mound"" in the vicinity of the licher field in Kansas and Oklahoma"

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US geological Survey Water Supply Paper, 2326. Sand waves, bars, and wind-blown, sand of the Rio Orinoco, Venezuela and Colombia / Nordin, C. F.

Public ISBD Titre de série : US geological Survey Water Supply Paper, 2326 Titre : Sand waves, bars, and wind-blown, sand of the Rio Orinoco, Venezuela and Colombia Type de document : texte imprimé Auteurs : Nordin, C. F. ; Perez-Hernadez, D. Mention d'édition : US Géological Survey, Federal Center Editeur : US geological Survey, Federal Center Année de publication : 1989 ISBN/ISSN/EAN : CI-05688 Note générale : This paper describes the particle size distributions of the bed samples and the concentrations of the suspended sediment samples that were collected during march 1982.Summarizes observations on the channel exposed during low flows and presents some approximate relations for estimating transport of sediment by wind and water Langues : Anglais (eng) Mots-clés : Hydrologie  Sable  Sediment  Transport Index. décimale : 551.48 Hydrologie : Résumé : This paper describes the particle size distributions of the bed samples and the concentrations of the suspended sediment samples that were collected during march 1982.Summarizes observations on the channel exposed during low flows and presents some approximate relations for estimating transport of sediment by wind and water Note de contenu : This paper describes the particle size distributions of the bed samples and the concentrations of the suspended sediment samples that were collected during march 1982.Summarizes observations on the channel exposed during low flows and presents some approximate relations for estimating transport of sediment by wind and water US geological Survey Water Supply Paper, 2326. Sand waves, bars, and wind-blown, sand of the Rio Orinoco, Venezuela and Colombia [texte imprimé] / Nordin, C. F. ; Perez-Hernadez, D.  . -  US Géological Survey, Federal Center . - US geological Survey, Federal Center, 1989. ISSN : CI-05688 This paper describes the particle size distributions of the bed samples and the concentrations of the suspended sediment samples that were collected during march 1982.Summarizes observations on the channel exposed during low flows and presents some approximate relations for estimating transport of sediment by wind and water Langues : Anglais (eng) Mots-clés : Hydrologie  Sable  Sediment  Transport Index. décimale : 551.48 Hydrologie : Résumé : This paper describes the particle size distributions of the bed samples and the concentrations of the suspended sediment samples that were collected during march 1982.Summarizes observations on the channel exposed during low flows and presents some approximate relations for estimating transport of sediment by wind and water Note de contenu : This paper describes the particle size distributions of the bed samples and the concentrations of the suspended sediment samples that were collected during march 1982.Summarizes observations on the channel exposed during low flows and presents some approximate relations for estimating transport of sediment by wind and water

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US geological Survey Water Supply Paper, 2337. Use of temperature profiles beneath streams to determine rates of vertical ground-water flow ans vertical hydraulic conductivity / Lapham, W. W.

Public ISBD Titre de série : US geological Survey Water Supply Paper, 2337 Titre : Use of temperature profiles beneath streams to determine rates of vertical ground-water flow ans vertical hydraulic conductivity Type de document : texte imprimé Auteurs : Lapham, W. W. Mention d'édition : US geological Survey, Federal Center Editeur : US geological Survey, Federal Center Année de publication : 1989 ISBN/ISSN/EAN : CI-05686 Note générale : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. Langues : Anglais (eng) Mots-clés : Température  Hydrogéologie  Eau souterraine  Sédiment  Conductivité hydraulique Index. décimale : 551.3 Phénomènes de surface et exogènes et leurs agents : érosion Résumé : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. Note de contenu : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. US geological Survey Water Supply Paper, 2337. Use of temperature profiles beneath streams to determine rates of vertical ground-water flow ans vertical hydraulic conductivity [texte imprimé] / Lapham, W. W.  . -  US geological Survey, Federal Center . - US geological Survey, Federal Center, 1989. ISSN : CI-05686 This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. Langues : Anglais (eng) Mots-clés : Température  Hydrogéologie  Eau souterraine  Sédiment  Conductivité hydraulique Index. décimale : 551.3 Phénomènes de surface et exogènes et leurs agents : érosion Résumé : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media. Note de contenu : This reports presents the results of a study, the principal objective of which was to evaluate the use of vertical temperature profiles in sediments beneath streams to determine rates of vertical ground-water flow and the effective vertical hydraulic conductivity of the sediments. The study included development of a numerical model based on a finite-difference approximation of stallman's (1963) equation describing the simultaneous flow of heat and fluid in porous media.

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US. Geological survey Water supply Paper, 2339. Guide for selecting manning's roughness coefficients for natural channels and flood plains / Arcement, G. J.

Public ISBD Titre de série : US. Geological survey Water supply Paper, 2339 Titre : Guide for selecting manning's roughness coefficients for natural channels and flood plains Type de document : texte imprimé Auteurs : Arcement, G. J. ; Schneider, V. R. Mention d'édition : US geological Survey, Federal Center Editeur : US geological Survey, Federal Center Année de publication : 1989 ISBN/ISSN/EAN : CI-05682 Note générale : Althougt much research has been done on manning roughness coefficient,n, for stream channels, very little has been done concerning the roughness values for densely vegetated flood plains. The n value is determined from the values of the factors that affect the roughness of channels and flood plains...Photographs of flood-plain segments where n values have been verified con be used as a comparison standard to aid in assigning n values to similar flood plains. Langues : Anglais (eng) Mots-clés : Hydrologie  Inondation  Végétation  Photographie  Ruissellement Index. décimale : 551.48 Hydrologie : Résumé : Althougt much research has been done on manning roughness coefficient,n, for stream channels, very little has been done concerning the roughness values for densely vegetated flood plains. The n value is determined from the values of the factors that affect the roughness of channels and flood plains...Photographs of flood-plain segments where n values have been verified con be used as a comparison standard to aid in assigning n values to similar flood plains. Note de contenu : Althougt much research has been done on manning roughness coefficient,n, for stream channels, very little has been done concerning the roughness values for densely vegetated flood plains. The n value is determined from the values of the factors that affect the roughness of channels and flood plains...Photographs of flood-plain segments where n values have been verified con be used as a comparison standard to aid in assigning n values to similar flood plains. US. Geological survey Water supply Paper, 2339. Guide for selecting manning's roughness coefficients for natural channels and flood plains [texte imprimé] / Arcement, G. J. ; Schneider, V. R.  . -  US geological Survey, Federal Center . - US geological Survey, Federal Center, 1989. ISSN : CI-05682 Althougt much research has been done on manning roughness coefficient,n, for stream channels, very little has been done concerning the roughness values for densely vegetated flood plains. The n value is determined from the values of the factors that affect the roughness of channels and flood plains...Photographs of flood-plain segments where n values have been verified con be used as a comparison standard to aid in assigning n values to similar flood plains. Langues : Anglais (eng) Mots-clés : Hydrologie  Inondation  Végétation  Photographie  Ruissellement Index. décimale : 551.48 Hydrologie : Résumé : Althougt much research has been done on manning roughness coefficient,n, for stream channels, very little has been done concerning the roughness values for densely vegetated flood plains. The n value is determined from the values of the factors that affect the roughness of channels and flood plains...Photographs of flood-plain segments where n values have been verified con be used as a comparison standard to aid in assigning n values to similar flood plains. Note de contenu : Althougt much research has been done on manning roughness coefficient,n, for stream channels, very little has been done concerning the roughness values for densely vegetated flood plains. The n value is determined from the values of the factors that affect the roughness of channels and flood plains...Photographs of flood-plain segments where n values have been verified con be used as a comparison standard to aid in assigning n values to similar flood plains.

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US geological Survey Water Supply Paper, 2345. Water movement in the unsaturated zone at a low-level radioactive-waste, Burial site near Barnvell, Gouth Carolina / Dennehy, K. F

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US geological Survey Water Supply Paper, 2358. Characteristics and trends of streamflow and dissolved solids in the Upper Colorado river bassin, Arizona, Colorado, New Mexico, Utah, and Wyoming / Liebermann, T. D.

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US geological Survey Water Supply Paper. Statiscal analysis relating well field to construction practices and siting of wells in the piedmont and blue ridge provinces of North Carolina / Daniel III, C. C.

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