U.S. Geological Survey Water Supply paper, 2286. Gas-film coefficients for the volatilization of ketones from water / Rathbun, R. E.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2286 Titre : Gas-film coefficients for the volatilization of ketones from water Type de document : texte imprimé Auteurs : Rathbun, R. E. ; Tai, D. Y. Mention d'édition : U. S. geological Survey Editeur : U. S. Geological Survey Année de publication : 1986 ISBN/ISSN/EAN : CI-05050 Note générale : Volatilization is a significant process in determining the fate of many organic compounds in treams and rivers. Quantifying this process requires knowledge of the mass-transfer coefficient from water, which is a function of the gas-film and liquid-film coefficients. The gas-film coefficient can be determined by seasuring the flux for the volatilization of pure organic liquids. Ten the report shows that the gas-film coefficient for acetone was much more dependent on temperature than more the coefficient for the other ketones. Langues : Anglais (eng) Mots-clés : Eau  Evaporation  Température  Hydrogène Index. décimale : 536.5 Température, Mesure des températures Résumé : Volatilization is a significant process in determining the fate of many organic compounds in treams and rivers. Quantifying this process requires knowledge of the mass-transfer coefficient from water, which is a function of the gas-film and liquid-film coefficients. The gas-film coefficient can be determined by seasuring the flux for the volatilization of pure organic liquids. Ten the report shows that the gas-film coefficient for acetone was much more dependent on temperature than more the coefficient for the other ketones. Note de contenu : Volatilization is a significant process in determining the fate of many organic compounds in treams and rivers. Quantifying this process requires knowledge of the mass-transfer coefficient from water, which is a function of the gas-film and liquid-film coefficients. The gas-film coefficient can be determined by seasuring the flux for the volatilization of pure organic liquids. Ten the report shows that the gas-film coefficient for acetone was much more dependent on temperature than more the coefficient for the other ketones. U.S. Geological Survey Water Supply paper, 2286. Gas-film coefficients for the volatilization of ketones from water [texte imprimé] / Rathbun, R. E. ; Tai, D. Y.  . -  U. S. geological Survey . - U. S. Geological Survey, 1986. ISSN : CI-05050 Volatilization is a significant process in determining the fate of many organic compounds in treams and rivers. Quantifying this process requires knowledge of the mass-transfer coefficient from water, which is a function of the gas-film and liquid-film coefficients. The gas-film coefficient can be determined by seasuring the flux for the volatilization of pure organic liquids. Ten the report shows that the gas-film coefficient for acetone was much more dependent on temperature than more the coefficient for the other ketones. Langues : Anglais (eng) Mots-clés : Eau  Evaporation  Température  Hydrogène Index. décimale : 536.5 Température, Mesure des températures Résumé : Volatilization is a significant process in determining the fate of many organic compounds in treams and rivers. Quantifying this process requires knowledge of the mass-transfer coefficient from water, which is a function of the gas-film and liquid-film coefficients. The gas-film coefficient can be determined by seasuring the flux for the volatilization of pure organic liquids. Ten the report shows that the gas-film coefficient for acetone was much more dependent on temperature than more the coefficient for the other ketones. Note de contenu : Volatilization is a significant process in determining the fate of many organic compounds in treams and rivers. Quantifying this process requires knowledge of the mass-transfer coefficient from water, which is a function of the gas-film and liquid-film coefficients. The gas-film coefficient can be determined by seasuring the flux for the volatilization of pure organic liquids. Ten the report shows that the gas-film coefficient for acetone was much more dependent on temperature than more the coefficient for the other ketones.

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U.S. Geological Survey Water Supply paper, 2290. Selected papers in the hydrologic sciences 1986 / Subitzky, S.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2290 Titre : Selected papers in the hydrologic sciences 1986 Type de document : texte imprimé Auteurs : Subitzky, S. Mention d'édition : U. S. Goverment Printing Office Editeur : U. S. Goverment Printing Office Année de publication : 1986 ISBN/ISSN/EAN : CI-05121 Note générale : This report is about limnology of west point reservoir and investigation of the possible formation of diethylnitrosamine resulting from the use of rhodamine WT dye as a tracer in river waters. Then it contains comparison of two stream discharge record reconstruction techniques for eight gaging stations in maine, evaluation of a suggest sequence for the chemical entraction of soluble amorphous phases from clays. Finally this study presents a preliminary evaluation of a discharge computation technique that uses a small number of velocity observations. Langues : Anglais (eng) Mots-clés : Hydrogéologie  Evaluation  Eau souterraine  Bassin versant  Hydrochimie  Limnologie Index. décimale : 551.48 Hydrologie : Résumé : This report is about limnology of west point reservoir and investigation of the possible formation of diethylnitrosamine resulting from the use of rhodamine WT dye as a tracer in river waters. Then it contains comparison of two stream discharge record reconstruction techniques for eight gaging stations in maine, evaluation of a suggest sequence for the chemical entraction of soluble amorphous phases from clays. Finally this study presents a preliminary evaluation of a discharge computation technique that uses a small number of velocity observations. Note de contenu : This report is about limnology of west point reservoir and investigation of the possible formation of diethylnitrosamine resulting from the use of rhodamine WT dye as a tracer in river waters. Then it contains comparison of two stream discharge record reconstruction techniques for eight gaging stations in maine, evaluation of a suggest sequence for the chemical entraction of soluble amorphous phases from clays. Finally this study presents a preliminary evaluation of a discharge computation technique that uses a small number of velocity observations. U.S. Geological Survey Water Supply paper, 2290. Selected papers in the hydrologic sciences 1986 [texte imprimé] / Subitzky, S.  . -  U. S. Goverment Printing Office . - U. S. Goverment Printing Office, 1986. ISSN : CI-05121 This report is about limnology of west point reservoir and investigation of the possible formation of diethylnitrosamine resulting from the use of rhodamine WT dye as a tracer in river waters. Then it contains comparison of two stream discharge record reconstruction techniques for eight gaging stations in maine, evaluation of a suggest sequence for the chemical entraction of soluble amorphous phases from clays. Finally this study presents a preliminary evaluation of a discharge computation technique that uses a small number of velocity observations. Langues : Anglais (eng) Mots-clés : Hydrogéologie  Evaluation  Eau souterraine  Bassin versant  Hydrochimie  Limnologie Index. décimale : 551.48 Hydrologie : Résumé : This report is about limnology of west point reservoir and investigation of the possible formation of diethylnitrosamine resulting from the use of rhodamine WT dye as a tracer in river waters. Then it contains comparison of two stream discharge record reconstruction techniques for eight gaging stations in maine, evaluation of a suggest sequence for the chemical entraction of soluble amorphous phases from clays. Finally this study presents a preliminary evaluation of a discharge computation technique that uses a small number of velocity observations. Note de contenu : This report is about limnology of west point reservoir and investigation of the possible formation of diethylnitrosamine resulting from the use of rhodamine WT dye as a tracer in river waters. Then it contains comparison of two stream discharge record reconstruction techniques for eight gaging stations in maine, evaluation of a suggest sequence for the chemical entraction of soluble amorphous phases from clays. Finally this study presents a preliminary evaluation of a discharge computation technique that uses a small number of velocity observations.

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U.S. Geological Survey Water Supply paper, 2299. Laboratory data on coarse-sediment transport for bedload-sampler calibrations / Hubbell, D. W.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2299 Titre : Laboratory data on coarse-sediment transport for bedload-sampler calibrations Type de document : texte imprimé Auteurs : Hubbell, D. W. ; Stevens, H. H. ; Skinner, J. V. Mention d'édition : U. S. Heological Survey, Federal Center Editeur : U. S. Heological Survey, Federal Center Année de publication : 1987 ISBN/ISSN/EAN : CI-05042 Note générale : A unique facility capable of recirculating and continuously measuring the transport rates of sediment particules ranging in size from about 1 to 75 millimeters in diameter was designed and used in an intensive program involving the calibration of bed load samplers. The facility consisted of a 9-foot-wide by 6-foot-deep by 272- - foot-long rectangular channel that incorporated seven automated collection pans accumulated, weighed and periodically dumped bed load falling through a shot in the channel floor. Tables indicate the extent of the data, which are avaitable on magnetic media ... Langues : Anglais (eng) Mots-clés : Sédiment  Eau de surface  Expérimentation  Hydrologie  Débit solide Index. décimale : 551.48 Hydrologie : Résumé : A unique facility capable of recirculating and continuously measuring the transport rates of sediment particules ranging in size from about 1 to 75 millimeters in diameter was designed and used in an intensive program involving the calibration of bed load samplers. The facility consisted of a 9-foot-wide by 6-foot-deep by 272- - foot-long rectangular channel that incorporated seven automated collection pans accumulated, weighed and periodically dumped bed load falling through a shot in the channel floor. Tables indicate the extent of the data, which are avaitable on magnetic media ... Note de contenu : A unique facility capable of recirculating and continuously measuring the transport rates of sediment particules ranging in size from about 1 to 75 millimeters in diameter was designed and used in an intensive program involving the calibration of bed load samplers. The facility consisted of a 9-foot-wide by 6-foot-deep by 272- - foot-long rectangular channel that incorporated seven automated collection pans accumulated, weighed and periodically dumped bed load falling through a shot in the channel floor. Tables indicate the extent of the data, which are avaitable on magnetic media ... U.S. Geological Survey Water Supply paper, 2299. Laboratory data on coarse-sediment transport for bedload-sampler calibrations [texte imprimé] / Hubbell, D. W. ; Stevens, H. H. ; Skinner, J. V.  . -  U. S. Heological Survey, Federal Center . - U. S. Heological Survey, Federal Center, 1987. ISSN : CI-05042 A unique facility capable of recirculating and continuously measuring the transport rates of sediment particules ranging in size from about 1 to 75 millimeters in diameter was designed and used in an intensive program involving the calibration of bed load samplers. The facility consisted of a 9-foot-wide by 6-foot-deep by 272- - foot-long rectangular channel that incorporated seven automated collection pans accumulated, weighed and periodically dumped bed load falling through a shot in the channel floor. Tables indicate the extent of the data, which are avaitable on magnetic media ... Langues : Anglais (eng) Mots-clés : Sédiment  Eau de surface  Expérimentation  Hydrologie  Débit solide Index. décimale : 551.48 Hydrologie : Résumé : A unique facility capable of recirculating and continuously measuring the transport rates of sediment particules ranging in size from about 1 to 75 millimeters in diameter was designed and used in an intensive program involving the calibration of bed load samplers. The facility consisted of a 9-foot-wide by 6-foot-deep by 272- - foot-long rectangular channel that incorporated seven automated collection pans accumulated, weighed and periodically dumped bed load falling through a shot in the channel floor. Tables indicate the extent of the data, which are avaitable on magnetic media ... Note de contenu : A unique facility capable of recirculating and continuously measuring the transport rates of sediment particules ranging in size from about 1 to 75 millimeters in diameter was designed and used in an intensive program involving the calibration of bed load samplers. The facility consisted of a 9-foot-wide by 6-foot-deep by 272- - foot-long rectangular channel that incorporated seven automated collection pans accumulated, weighed and periodically dumped bed load falling through a shot in the channel floor. Tables indicate the extent of the data, which are avaitable on magnetic media ...

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U.S. Geological Survey Water Supply paper, 2305. Sources of coal-mine drainage an their effects on surface-water chemistry in the claybank creek basin and vicinity, north-central Missouri, 1983 - 84 / Blevins, D. W.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2305 Titre : Sources of coal-mine drainage an their effects on surface-water chemistry in the claybank creek basin and vicinity, north-central Missouri, 1983 - 84 Type de document : texte imprimé Auteurs : Blevins, D. W. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1989 ISBN/ISSN/EAN : CI-05080 Note générale : Eighteen sources of drainage related to past coal-mining activity were identified in the Claybank Creek, Missouri, study area, and eight of them were considered large enough to have detectable effects on receiving streams. However, only three sources significantly affected the chemistry of water in receiving streams. Most underground mines in the North Fork Claybank Creek basin seem to be hydraulically connected, and about 80 percent of their discharge surfaced at one site. Drainage from the underground mines contributed most of the dissolved constituents in north Fork Claybank Creek during dry water. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrochimie  Eau de surface  Qualité de l'eau  Drainage Index. décimale : 621.2 Hydraulique : turbines, pompes, accumulateurs, transmission hydraulique Résumé : Eighteen sources of drainage related to past coal-mining activity were identified in the Claybank Creek, Missouri, study area, and eight of them were considered large enough to have detectable effects on receiving streams. However, only three sources significantly affected the chemistry of water in receiving streams. Most underground mines in the North Fork Claybank Creek basin seem to be hydraulically connected, and about 80 percent of their discharge surfaced at one site. Drainage from the underground mines contributed most of the dissolved constituents in north Fork Claybank Creek during dry water. Note de contenu : Eighteen sources of drainage related to past coal-mining activity were identified in the Claybank Creek, Missouri, study area, and eight of them were considered large enough to have detectable effects on receiving streams. However, only three sources significantly affected the chemistry of water in receiving streams. Most underground mines in the North Fork Claybank Creek basin seem to be hydraulically connected, and about 80 percent of their discharge surfaced at one site. Drainage from the underground mines contributed most of the dissolved constituents in north Fork Claybank Creek during dry water. U.S. Geological Survey Water Supply paper, 2305. Sources of coal-mine drainage an their effects on surface-water chemistry in the claybank creek basin and vicinity, north-central Missouri, 1983 - 84 [texte imprimé] / Blevins, D. W.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1989. ISSN : CI-05080 Eighteen sources of drainage related to past coal-mining activity were identified in the Claybank Creek, Missouri, study area, and eight of them were considered large enough to have detectable effects on receiving streams. However, only three sources significantly affected the chemistry of water in receiving streams. Most underground mines in the North Fork Claybank Creek basin seem to be hydraulically connected, and about 80 percent of their discharge surfaced at one site. Drainage from the underground mines contributed most of the dissolved constituents in north Fork Claybank Creek during dry water. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrochimie  Eau de surface  Qualité de l'eau  Drainage Index. décimale : 621.2 Hydraulique : turbines, pompes, accumulateurs, transmission hydraulique Résumé : Eighteen sources of drainage related to past coal-mining activity were identified in the Claybank Creek, Missouri, study area, and eight of them were considered large enough to have detectable effects on receiving streams. However, only three sources significantly affected the chemistry of water in receiving streams. Most underground mines in the North Fork Claybank Creek basin seem to be hydraulically connected, and about 80 percent of their discharge surfaced at one site. Drainage from the underground mines contributed most of the dissolved constituents in north Fork Claybank Creek during dry water. Note de contenu : Eighteen sources of drainage related to past coal-mining activity were identified in the Claybank Creek, Missouri, study area, and eight of them were considered large enough to have detectable effects on receiving streams. However, only three sources significantly affected the chemistry of water in receiving streams. Most underground mines in the North Fork Claybank Creek basin seem to be hydraulically connected, and about 80 percent of their discharge surfaced at one site. Drainage from the underground mines contributed most of the dissolved constituents in north Fork Claybank Creek during dry water.

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U.S. Geological Survey Water Supply paper, 2309. Quantitative assessment of the shallow ground-water flow system associated with Connetquot Brook, Long Island, New York / Prince, K. R.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2309 Titre : Quantitative assessment of the shallow ground-water flow system associated with Connetquot Brook, Long Island, New York Type de document : texte imprimé Auteurs : Prince, K. R. ; Franke, L. O. ; Reilly, T. E. Mention d'édition : United States Gouvernement Printing Office Editeur : United States Gouvernement Printing Office Année de publication : 1988 ISBN/ISSN/EAN : CI-05081 Note générale : Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. Langues : Anglais (eng) Mots-clés : Eau souterraine  Bassin versant  Drainage  Hydrochimie  Mesure et observation  Météorologie  Simulation  Evaluation quantitative Index. décimale : 551.48 Hydrologie : Résumé : Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. Note de contenu : Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. U.S. Geological Survey Water Supply paper, 2309. Quantitative assessment of the shallow ground-water flow system associated with Connetquot Brook, Long Island, New York [texte imprimé] / Prince, K. R. ; Franke, L. O. ; Reilly, T. E.  . -  United States Gouvernement Printing Office . - United States Gouvernement Printing Office, 1988. ISSN : CI-05081 Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. Langues : Anglais (eng) Mots-clés : Eau souterraine  Bassin versant  Drainage  Hydrochimie  Mesure et observation  Météorologie  Simulation  Evaluation quantitative Index. décimale : 551.48 Hydrologie : Résumé : Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream. Note de contenu : Streamflow on Long Island is derived principally from shallow ground water that flows above the deeper regional flow system. The movement of shallow ground water was studied during 1975-82 at Connetquot Brook, an undisturbed stream in Connetquot River State Park, in south-central Long Island, New York. The investigation encompassed (1) field studies of streamflow, ground-water levels, and age of water as indicated by tritium and dissolved-oxygen concentration an (2) numerical simulation of the shallow flow system to evaluate the hydraulic factors that govern the direction of shallow ground-water flow near and beneath the stream.

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U.S. Geological Survey Water Supply paper, 2311. Specific conductance : theoretical considerations and application to analytical quality control / Miller, D. L.

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U.S. Geological Survey Water Supply paper, 2315. The effects of boundary conditions on the steady-state response of three hypothetical ground-water systems results and implications of numerical experiments / Franke, L. O.

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U.S. Geological Survey Water Supply paper, 2319. Effect of water quality on survival of Lahontan Cutthroat trout eggs in the Truckee River, West-central Nevada and Estern California / Hoffman, R. J.

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U.S. Geological Survey Water Supply paper, 2323. Aqueous geochemistry of the Magothy aquifer, Maryland / Knobel, L. L.

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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.

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U.S. Geological Survey Water Supply paper, 2328. A well system to recover usable water from a freshwater - saltwater aquifer in Puerto Rico / Zack, A. L.

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U.S. Geological Survey Water Supply paper, 2330. Selected in the hydrologic sciences 1987 / Subitzky, S.

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U.S. Geological Survey Water Supply paper, 2331. Simulation of saltwater movement in the floridan system, Hilton Head Island, South Carolina / Bush, P. W.

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U.S. Geological Survey Water Supply paper, 2333. Tritium migration from a low-level radioactive-waste disposal site near Chicago, Illinois / Nicholas, J. R.

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U.S. Geological Survey Water Supply paper, 2335. Rainfall and runoff quantity and quality characteristics of four urban land-use catchments in Fresno, California, october 1981 to april 1983 / Altmann, R. N.

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