U.S. Geological Survey Water Supply paper, 2203. Investigation of the flooding in the Tug Fork Basin of Kentucky Virginia and West Virginia / Hirsch, R. M.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2203 Titre : Investigation of the flooding in the Tug Fork Basin of Kentucky Virginia and West Virginia Type de document : texte imprimé Auteurs : Hirsch, R. M. ; Scott, A. G. ; Wyant, T. Mention d'édition : U. S. Geological Survey Editeur : U. S. Geological Survey Année de publication : 1982 ISBN/ISSN/EAN : CI-05099 Note générale : "Statistical analysis indicates that the average size of annual-flood peaks of the Tug Fork has been increasing. However, additional statistical analysis does not indicate that the flood levels that were exceeded typically once or twice a year in the period 1947 - 79 are any more likely to be exceeded now than in 1947. Possible trends in stream-channel size also are investigated at three locations. No discernible trends in channel size are noted. Further statistical analysis of the trend in the size of annual-flood peaks shows that much of the annual variation is related to local rainfall and to the ""natrual"" hydrologic response in a relatively undisturbed subbasin. However, some statistical indication of trend persists after accounting for these natural factors, though it is of borderline statistical significance." Langues : Anglais (eng) Mots-clés : Hydrologie  Eau de surface  Inondation  Bassin versant  Crue  PRECIPITATIONS Index. décimale : 551.48 Hydrologie : Résumé : "Statistical analysis indicates that the average size of annual-flood peaks of the Tug Fork has been increasing. However, additional statistical analysis does not indicate that the flood levels that were exceeded typically once or twice a year in the period 1947 - 79 are any more likely to be exceeded now than in 1947. Possible trends in stream-channel size also are investigated at three locations. No discernible trends in channel size are noted. Further statistical analysis of the trend in the size of annual-flood peaks shows that much of the annual variation is related to local rainfall and to the ""natrual"" hydrologic response in a relatively undisturbed subbasin. However, some statistical indication of trend persists after accounting for these natural factors, though it is of borderline statistical significance." Note de contenu : "Statistical analysis indicates that the average size of annual-flood peaks of the Tug Fork has been increasing. However, additional statistical analysis does not indicate that the flood levels that were exceeded typically once or twice a year in the period 1947 - 79 are any more likely to be exceeded now than in 1947. Possible trends in stream-channel size also are investigated at three locations. No discernible trends in channel size are noted. Further statistical analysis of the trend in the size of annual-flood peaks shows that much of the annual variation is related to local rainfall and to the ""natrual"" hydrologic response in a relatively undisturbed subbasin. However, some statistical indication of trend persists after accounting for these natural factors, though it is of borderline statistical significance." U.S. Geological Survey Water Supply paper, 2203. Investigation of the flooding in the Tug Fork Basin of Kentucky Virginia and West Virginia [texte imprimé] / Hirsch, R. M. ; Scott, A. G. ; Wyant, T.  . -  U. S. Geological Survey . - U. S. Geological Survey, 1982. ISSN : CI-05099 "Statistical analysis indicates that the average size of annual-flood peaks of the Tug Fork has been increasing. However, additional statistical analysis does not indicate that the flood levels that were exceeded typically once or twice a year in the period 1947 - 79 are any more likely to be exceeded now than in 1947. Possible trends in stream-channel size also are investigated at three locations. No discernible trends in channel size are noted. Further statistical analysis of the trend in the size of annual-flood peaks shows that much of the annual variation is related to local rainfall and to the ""natrual"" hydrologic response in a relatively undisturbed subbasin. However, some statistical indication of trend persists after accounting for these natural factors, though it is of borderline statistical significance." Langues : Anglais (eng) Mots-clés : Hydrologie  Eau de surface  Inondation  Bassin versant  Crue  PRECIPITATIONS Index. décimale : 551.48 Hydrologie : Résumé : "Statistical analysis indicates that the average size of annual-flood peaks of the Tug Fork has been increasing. However, additional statistical analysis does not indicate that the flood levels that were exceeded typically once or twice a year in the period 1947 - 79 are any more likely to be exceeded now than in 1947. Possible trends in stream-channel size also are investigated at three locations. No discernible trends in channel size are noted. Further statistical analysis of the trend in the size of annual-flood peaks shows that much of the annual variation is related to local rainfall and to the ""natrual"" hydrologic response in a relatively undisturbed subbasin. However, some statistical indication of trend persists after accounting for these natural factors, though it is of borderline statistical significance." Note de contenu : "Statistical analysis indicates that the average size of annual-flood peaks of the Tug Fork has been increasing. However, additional statistical analysis does not indicate that the flood levels that were exceeded typically once or twice a year in the period 1947 - 79 are any more likely to be exceeded now than in 1947. Possible trends in stream-channel size also are investigated at three locations. No discernible trends in channel size are noted. Further statistical analysis of the trend in the size of annual-flood peaks shows that much of the annual variation is related to local rainfall and to the ""natrual"" hydrologic response in a relatively undisturbed subbasin. However, some statistical indication of trend persists after accounting for these natural factors, though it is of borderline statistical significance."

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U.S. Geological Survey Water Supply paper, 2204. Characterization of mineral precipitates by electron microscope photographs and electron diffraction patterns / Lind, C. J.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2204 Titre : Characterization of mineral precipitates by electron microscope photographs and electron diffraction patterns Type de document : texte imprimé Auteurs : Lind, C. J. Mention d'édition : U. S. Geological Survey Editeur : U. S. Geological Survey Année de publication : 1983 ISBN/ISSN/EAN : CI-05100 Note générale : Transmission electron micrographs and electron diffraction techniques can be used to characterize microcrystalline precipitates too minute for characterization by x-ray diffraction. Included is a description of the electron microscope, explanations of sample preparation and diffraction pattern interpretation and examples of electron micrograph and electron diffractions applications and their limitations. The techniques applied to preparations of manganese oxides, show the development of crystallinity and the change in crystal form with aging... Langues : Anglais (eng) Mots-clés : Minéralogie  Expérimentation  Electron  Physique Index. décimale : 551.48 Hydrologie : Résumé : Transmission electron micrographs and electron diffraction techniques can be used to characterize microcrystalline precipitates too minute for characterization by x-ray diffraction. Included is a description of the electron microscope, explanations of sample preparation and diffraction pattern interpretation and examples of electron micrograph and electron diffractions applications and their limitations. The techniques applied to preparations of manganese oxides, show the development of crystallinity and the change in crystal form with aging... Note de contenu : Transmission electron micrographs and electron diffraction techniques can be used to characterize microcrystalline precipitates too minute for characterization by x-ray diffraction. Included is a description of the electron microscope, explanations of sample preparation and diffraction pattern interpretation and examples of electron micrograph and electron diffractions applications and their limitations. The techniques applied to preparations of manganese oxides, show the development of crystallinity and the change in crystal form with aging... U.S. Geological Survey Water Supply paper, 2204. Characterization of mineral precipitates by electron microscope photographs and electron diffraction patterns [texte imprimé] / Lind, C. J.  . -  U. S. Geological Survey . - U. S. Geological Survey, 1983. ISSN : CI-05100 Transmission electron micrographs and electron diffraction techniques can be used to characterize microcrystalline precipitates too minute for characterization by x-ray diffraction. Included is a description of the electron microscope, explanations of sample preparation and diffraction pattern interpretation and examples of electron micrograph and electron diffractions applications and their limitations. The techniques applied to preparations of manganese oxides, show the development of crystallinity and the change in crystal form with aging... Langues : Anglais (eng) Mots-clés : Minéralogie  Expérimentation  Electron  Physique Index. décimale : 551.48 Hydrologie : Résumé : Transmission electron micrographs and electron diffraction techniques can be used to characterize microcrystalline precipitates too minute for characterization by x-ray diffraction. Included is a description of the electron microscope, explanations of sample preparation and diffraction pattern interpretation and examples of electron micrograph and electron diffractions applications and their limitations. The techniques applied to preparations of manganese oxides, show the development of crystallinity and the change in crystal form with aging... Note de contenu : Transmission electron micrographs and electron diffraction techniques can be used to characterize microcrystalline precipitates too minute for characterization by x-ray diffraction. Included is a description of the electron microscope, explanations of sample preparation and diffraction pattern interpretation and examples of electron micrograph and electron diffractions applications and their limitations. The techniques applied to preparations of manganese oxides, show the development of crystallinity and the change in crystal form with aging...

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U.S. Geological Survey Water Supply paper, 2206. Simulation of an aquifer test on the Tesuque Pueblo Grant, New Mexico / Hearne, G. A.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2206 Titre : Simulation of an aquifer test on the Tesuque Pueblo Grant, 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-05102 Note générale : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrogéologie  Géophysique  Simulation  Modélisation Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. Note de contenu : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. U.S. Geological Survey Water Supply paper, 2206. Simulation of an aquifer test on the Tesuque Pueblo Grant, New Mexico [texte imprimé] / Hearne, G. A.  . -  U. S. Geological survey . - U. S. Geological Survey, 1985. ISSN : CI-05102 An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. Langues : Anglais (eng) Mots-clés : Bassin versant  Hydrogéologie  Géophysique  Simulation  Modélisation Index. décimale : 551 Géologie, météorologie, hydrologie générale Résumé : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis. Note de contenu : An aquifer test was designed and conducted in the anisotronic dipping beds of the Tesuque formation on the Tesuque Pueblo Grant, New Mexico. This report describes the design execution ans analysis of the aquifer test. The aquifer system tested consists of interbedded permeable and less permeable layers which dip from the horizontal. Flow through the aquifer systems is such that the hydraulic heads are higher in the deeper beds. These boundary and initial conditions dictate the method required for analysis.

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U.S. Geological Survey Water Supply paper, 2207. Flood characteristic of urban watersheds in the United States / Sauer, V. B.

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2207 Titre : Flood characteristic of urban watersheds in the United States Type de document : texte imprimé Auteurs : Sauer, V. B. ; Thomas, W. O. ; Stricker, V. A. Mention d'édition : United States Gouverment Printing Office Editeur : United States Gouverment Printing Office Année de publication : 1983 ISBN/ISSN/EAN : CI-05118 Note générale : With urban grouwth and development, there is an ever-increasing need for flood information and estimating techniques in areas where little or no data exist. In 1978, the Federal Highway Administration, Department of Transportation (FHWA) contracted with the Geological Survey to make a nationwide study of urban flood frequency. The purposes of the study were (1) to review the literature of urban flood studies/ (2) to compile a nationwide data base of flood-frequency characteristics, topographic, physical, and climatic characteristics/ and land-use variables for as many urbanized watersheds as possible/ and (3) to definie estimating techniques that could be used in ungaged urban areas/ This report describe the results of that study. Langues : Anglais (eng) Mots-clés : Urbanisme  Inondation  Ruissellement  Mesure et observation  Méthodologie Index. décimale : 711 Urbanisme. Aménagement du territoire Résumé : With urban grouwth and development, there is an ever-increasing need for flood information and estimating techniques in areas where little or no data exist. In 1978, the Federal Highway Administration, Department of Transportation (FHWA) contracted with the Geological Survey to make a nationwide study of urban flood frequency. The purposes of the study were (1) to review the literature of urban flood studies/ (2) to compile a nationwide data base of flood-frequency characteristics, topographic, physical, and climatic characteristics/ and land-use variables for as many urbanized watersheds as possible/ and (3) to definie estimating techniques that could be used in ungaged urban areas/ This report describe the results of that study. Note de contenu : With urban grouwth and development, there is an ever-increasing need for flood information and estimating techniques in areas where little or no data exist. In 1978, the Federal Highway Administration, Department of Transportation (FHWA) contracted with the Geological Survey to make a nationwide study of urban flood frequency. The purposes of the study were (1) to review the literature of urban flood studies/ (2) to compile a nationwide data base of flood-frequency characteristics, topographic, physical, and climatic characteristics/ and land-use variables for as many urbanized watersheds as possible/ and (3) to definie estimating techniques that could be used in ungaged urban areas/ This report describe the results of that study. U.S. Geological Survey Water Supply paper, 2207. Flood characteristic of urban watersheds in the United States [texte imprimé] / Sauer, V. B. ; Thomas, W. O. ; Stricker, V. A.  . -  United States Gouverment Printing Office . - United States Gouverment Printing Office, 1983. ISSN : CI-05118 With urban grouwth and development, there is an ever-increasing need for flood information and estimating techniques in areas where little or no data exist. In 1978, the Federal Highway Administration, Department of Transportation (FHWA) contracted with the Geological Survey to make a nationwide study of urban flood frequency. The purposes of the study were (1) to review the literature of urban flood studies/ (2) to compile a nationwide data base of flood-frequency characteristics, topographic, physical, and climatic characteristics/ and land-use variables for as many urbanized watersheds as possible/ and (3) to definie estimating techniques that could be used in ungaged urban areas/ This report describe the results of that study. Langues : Anglais (eng) Mots-clés : Urbanisme  Inondation  Ruissellement  Mesure et observation  Méthodologie Index. décimale : 711 Urbanisme. Aménagement du territoire Résumé : With urban grouwth and development, there is an ever-increasing need for flood information and estimating techniques in areas where little or no data exist. In 1978, the Federal Highway Administration, Department of Transportation (FHWA) contracted with the Geological Survey to make a nationwide study of urban flood frequency. The purposes of the study were (1) to review the literature of urban flood studies/ (2) to compile a nationwide data base of flood-frequency characteristics, topographic, physical, and climatic characteristics/ and land-use variables for as many urbanized watersheds as possible/ and (3) to definie estimating techniques that could be used in ungaged urban areas/ This report describe the results of that study. Note de contenu : With urban grouwth and development, there is an ever-increasing need for flood information and estimating techniques in areas where little or no data exist. In 1978, the Federal Highway Administration, Department of Transportation (FHWA) contracted with the Geological Survey to make a nationwide study of urban flood frequency. The purposes of the study were (1) to review the literature of urban flood studies/ (2) to compile a nationwide data base of flood-frequency characteristics, topographic, physical, and climatic characteristics/ and land-use variables for as many urbanized watersheds as possible/ and (3) to definie estimating techniques that could be used in ungaged urban areas/ This report describe the results of that study.

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

Public ISBD Titre de série : U.S. Geological Survey Water Supply paper, 2208 Titre : Streamflow augmentation at fosters brook, Long island, New York - A hydraulic feasability study Type de document : texte imprimé Auteurs : Prince, K. R. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1984 ISBN/ISSN/EAN : CI-05071 Note générale : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. Langues : Anglais (eng) Mots-clés : Eau de surface  Eau souterraine  Infiltration  Hydrochimie  Température de l'eau  Modèle numérique Index. décimale : 551.48 Hydrologie : Résumé : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. Note de contenu : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. U.S. Geological Survey Water Supply paper, 2208. Streamflow augmentation at fosters brook, Long island, New York - A hydraulic feasability study [texte imprimé] / Prince, K. R.  . -  United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1984. ISSN : CI-05071 A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. Langues : Anglais (eng) Mots-clés : Eau de surface  Eau souterraine  Infiltration  Hydrochimie  Température de l'eau  Modèle numérique Index. décimale : 551.48 Hydrologie : Résumé : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours. Note de contenu : A 27 day streamflow augmentation test was conducted in december 1979 at fosters brook, near the south shore of long Island, to investigate the hydraulic feasibility of pumping ground water to supply flow to an ephemeral stream during dry periods. Measurements of soil moisture in the unsaturated zone beneath the streambed indicate that infiltration rate and soil-moisture content are interrelated. Initial infiltration was measured with a neutron logger/ the wetting front traversed the unsaturated zone at an average of 11.2 inches per hour and reached the water table in 5.5 hours.

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

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

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U.S. Geological Survey Water Supply paper, 2216. Daily water and sediment discharges from selected rivers of the eastern United States : a time-series modeling approach / Fitzgerald, M. G.

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

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

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

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U.S. Geological Survey Water Supply paper, 2221. Hydrology of major estuaries and sounds of north Carolina / Giese, G. L.

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U.S. Geological Survey Water Supply paper, 2223. Floods of october 1977 in southern Arizona and march 1978 in Central Arizona / Aldridge, B. N.

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U.S. Geological Survey Water Supply paper, 2225. Traveltimes of flood waves on the neuw river between Hinton and hawks nest, west Virginia / Appel, D. H.

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U.S. Geological Survey Water Supply paper, 2226. Low-level radioactive - Waste burial at the Palos Forest Preserve, Illinois : Geology and hydrology of the glacial dript as related to the migration of tritium / Olimpio, J. C.

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