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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.
Titre de série : U.S. Geological Survey Water Supply paper, 2216 Titre : Daily water and sediment discharges from selected rivers of the eastern United States : a time-series modeling approach Type de document : texte imprimé Auteurs : Fitzgerald, M. G. ; Karkinger, M. R. ; Michael, R Mention d'édition : United States Gouvernement Printing Office Editeur : United States Gouvernement Printing Office Année de publication : 14983 ISBN/ISSN/EAN : CI-05064 Note générale : Time-series models were constructed for analysis of daily runoff and sediment discharge data from selected rivers of the eastern United States. Logarithmic transformation and first order differencing of the data sets were necessary to produce second order stationary time series and remove seasonal trends. Cyclic models accounted for less than 42 percent in the sediment series. Analysis of the apparent oscillations of given frequenciers occuring in the data indicates that frequently occuring storms can account for as much as 50 percent of the variation in sediment dischange. Langues : Anglais (eng) Mots-clés : Ruissellement Sédimentation Débit solide Eau de surface Index. décimale : 551.48 Hydrologie : Résumé : Time-series models were constructed for analysis of daily runoff and sediment discharge data from selected rivers of the eastern United States. Logarithmic transformation and first order differencing of the data sets were necessary to produce second order stationary time series and remove seasonal trends. Cyclic models accounted for less than 42 percent in the sediment series. Analysis of the apparent oscillations of given frequenciers occuring in the data indicates that frequently occuring storms can account for as much as 50 percent of the variation in sediment dischange. Note de contenu : Time-series models were constructed for analysis of daily runoff and sediment discharge data from selected rivers of the eastern United States. Logarithmic transformation and first order differencing of the data sets were necessary to produce second order stationary time series and remove seasonal trends. Cyclic models accounted for less than 42 percent in the sediment series. Analysis of the apparent oscillations of given frequenciers occuring in the data indicates that frequently occuring storms can account for as much as 50 percent of the variation in sediment dischange. 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 [texte imprimé] / Fitzgerald, M. G. ; Karkinger, M. R. ; Michael, R . - United States Gouvernement Printing Office . - United States Gouvernement Printing Office, 14983.
ISSN : CI-05064
Time-series models were constructed for analysis of daily runoff and sediment discharge data from selected rivers of the eastern United States. Logarithmic transformation and first order differencing of the data sets were necessary to produce second order stationary time series and remove seasonal trends. Cyclic models accounted for less than 42 percent in the sediment series. Analysis of the apparent oscillations of given frequenciers occuring in the data indicates that frequently occuring storms can account for as much as 50 percent of the variation in sediment dischange.
Langues : Anglais (eng)
Mots-clés : Ruissellement Sédimentation Débit solide Eau de surface Index. décimale : 551.48 Hydrologie : Résumé : Time-series models were constructed for analysis of daily runoff and sediment discharge data from selected rivers of the eastern United States. Logarithmic transformation and first order differencing of the data sets were necessary to produce second order stationary time series and remove seasonal trends. Cyclic models accounted for less than 42 percent in the sediment series. Analysis of the apparent oscillations of given frequenciers occuring in the data indicates that frequently occuring storms can account for as much as 50 percent of the variation in sediment dischange. Note de contenu : Time-series models were constructed for analysis of daily runoff and sediment discharge data from selected rivers of the eastern United States. Logarithmic transformation and first order differencing of the data sets were necessary to produce second order stationary time series and remove seasonal trends. Cyclic models accounted for less than 42 percent in the sediment series. Analysis of the apparent oscillations of given frequenciers occuring in the data indicates that frequently occuring storms can account for as much as 50 percent of the variation in sediment dischange. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B064.184698 CI-05064 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B064.184697 CI-05064 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B064.184696 CI-05064 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B064.184695 CI-05064 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B064.184694 CI-05064 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B064.184693 CI-05064 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B064.184692 CI-05064 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B064.184691 CI-05064 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U.S. Geological Survey Water Supply paper, 2218. Sewage plume in a sand and gravel aquifer, Cape cod, Massachusetts / Le Blanc, D. R.
Titre de série : U.S. Geological Survey Water Supply paper, 2218 Titre : Sewage plume in a sand and gravel aquifer, Cape cod, Massachusetts Type de document : texte imprimé Auteurs : Le Blanc, D. R. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1984 ISBN/ISSN/EAN : CI-05066 Note générale : A plume of contamined ground water has been formed by 45 years of disposal of treated sewage to a sand and gravel aquifer at Otis AFB. The secondarily treated sewage is recharged to the aquifer by rapid infiltration through sand beds. The plume extends more than 11,000 feet to 3,500 feet wide and 75 feet thick. The plume is contained primarily in the 90 to 140 foot-ticks permeable sand and gravel that overlies less permeable fine-grained sediments. The plume is overlain by 20 to 50 feet of uncontamination ground water. Langues : Anglais (eng) Mots-clés : Bassin versant Eau souterraine Qualité de l'eau Hydrogéologie Hydrologie Hydrochimie Eau usée Contamination de l'eau Index. décimale : 551.48 Hydrologie : Résumé : A plume of contamined ground water has been formed by 45 years of disposal of treated sewage to a sand and gravel aquifer at Otis AFB. The secondarily treated sewage is recharged to the aquifer by rapid infiltration through sand beds. The plume extends more than 11,000 feet to 3,500 feet wide and 75 feet thick. The plume is contained primarily in the 90 to 140 foot-ticks permeable sand and gravel that overlies less permeable fine-grained sediments. The plume is overlain by 20 to 50 feet of uncontamination ground water. Note de contenu : A plume of contamined ground water has been formed by 45 years of disposal of treated sewage to a sand and gravel aquifer at Otis AFB. The secondarily treated sewage is recharged to the aquifer by rapid infiltration through sand beds. The plume extends more than 11,000 feet to 3,500 feet wide and 75 feet thick. The plume is contained primarily in the 90 to 140 foot-ticks permeable sand and gravel that overlies less permeable fine-grained sediments. The plume is overlain by 20 to 50 feet of uncontamination ground water. U.S. Geological Survey Water Supply paper, 2218. Sewage plume in a sand and gravel aquifer, Cape cod, Massachusetts [texte imprimé] / Le Blanc, D. R. . - United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1984.
ISSN : CI-05066
A plume of contamined ground water has been formed by 45 years of disposal of treated sewage to a sand and gravel aquifer at Otis AFB. The secondarily treated sewage is recharged to the aquifer by rapid infiltration through sand beds. The plume extends more than 11,000 feet to 3,500 feet wide and 75 feet thick. The plume is contained primarily in the 90 to 140 foot-ticks permeable sand and gravel that overlies less permeable fine-grained sediments. The plume is overlain by 20 to 50 feet of uncontamination ground water.
Langues : Anglais (eng)
Mots-clés : Bassin versant Eau souterraine Qualité de l'eau Hydrogéologie Hydrologie Hydrochimie Eau usée Contamination de l'eau Index. décimale : 551.48 Hydrologie : Résumé : A plume of contamined ground water has been formed by 45 years of disposal of treated sewage to a sand and gravel aquifer at Otis AFB. The secondarily treated sewage is recharged to the aquifer by rapid infiltration through sand beds. The plume extends more than 11,000 feet to 3,500 feet wide and 75 feet thick. The plume is contained primarily in the 90 to 140 foot-ticks permeable sand and gravel that overlies less permeable fine-grained sediments. The plume is overlain by 20 to 50 feet of uncontamination ground water. Note de contenu : A plume of contamined ground water has been formed by 45 years of disposal of treated sewage to a sand and gravel aquifer at Otis AFB. The secondarily treated sewage is recharged to the aquifer by rapid infiltration through sand beds. The plume extends more than 11,000 feet to 3,500 feet wide and 75 feet thick. The plume is contained primarily in the 90 to 140 foot-ticks permeable sand and gravel that overlies less permeable fine-grained sediments. The plume is overlain by 20 to 50 feet of uncontamination ground water. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B066.82241 CI-05066 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B066.82242 CI-05066 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B066.82240 CI-05066 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B066.82238 CI-05066 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B066.82239 CI-05066 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B066.82237 CI-05066 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B066.82235 CI-05066 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B066.82236 CI-05066 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible 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.
Titre de série : U.S. Geological Survey Water Supply paper, 2219 Titre : Hydrogeologic setting and the potentiometric surfaces of regional aquifers in the Hollandale embayment, southeastern Minnesota, 1970 - 80 Type de document : texte imprimé Auteurs : Delin, G. N. ; Woodward, D. G. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1984 ISBN/ISSN/EAN : CI-05067 Note générale : Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. Langues : Anglais (eng) Mots-clés : Hydrogéologie Bassin versant Eau souterraine PRECIPITATIONS Index. décimale : 551.48 Hydrologie : Résumé : Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. Note de contenu : Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. 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 [texte imprimé] / Delin, G. N. ; Woodward, D. G. . - United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1984.
ISSN : CI-05067
Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa.
Langues : Anglais (eng)
Mots-clés : Hydrogéologie Bassin versant Eau souterraine PRECIPITATIONS Index. décimale : 551.48 Hydrologie : Résumé : Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. Note de contenu : Sedimentary paleozoic rocks in the Hollandale embayment in southeastern Minnesota are as thick as 2,000 ft. This sedimentary sequence, together with the proterozoic hinckley sandstone and the quaternary drift, is divided into six regional aquifers : undifferentiated drift, upper carbonate, St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley. Potentiometric-surface maps for each aquifer indicate that mouvement of ground water is predominatly toward the major rivers. The St. Croix, Minnesota, and Mississipu rivers constitute regional discharge boundaries for ground water flow. A majoor ground-water divide in the St. Peter, Prairie du chien-Jordan, Iranton-Galesville, and Mount Simon-Hinckley aquifers in the south-central part of the Hollandale embayment separates ground-water flow northward toward the twin cities area and southward toward Iowa. Réservation
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Titre de série : U.S. Geological Survey Water Supply paper, 2220 Titre : Basic ground-water hydrology Type de document : texte imprimé Auteurs : Heath, R. C. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1983 ISBN/ISSN/EAN : CI-05068 Note générale : Each section consists of a brief text and one or more drawings or maps that illustrate the main points covered in the text. Because the text is, in effect, an expanded discussion of the illustrations, most of the illustrations are not captioned. However, where more than one drawing is included in a section, each drawing is assigned a number, given in parentheses, and these numbers are inserted at places in the text where the reader should refer to the drawing. Langues : Anglais (eng) Mots-clés : Eau souterraine Cycle de l'eau Topographie Qualité de l'eau Pollution Température Index. décimale : 551.48 Hydrologie : Résumé : Each section consists of a brief text and one or more drawings or maps that illustrate the main points covered in the text. Because the text is, in effect, an expanded discussion of the illustrations, most of the illustrations are not captioned. However, where more than one drawing is included in a section, each drawing is assigned a number, given in parentheses, and these numbers are inserted at places in the text where the reader should refer to the drawing. Note de contenu : Each section consists of a brief text and one or more drawings or maps that illustrate the main points covered in the text. Because the text is, in effect, an expanded discussion of the illustrations, most of the illustrations are not captioned. However, where more than one drawing is included in a section, each drawing is assigned a number, given in parentheses, and these numbers are inserted at places in the text where the reader should refer to the drawing. U.S. Geological Survey Water Supply paper, 2220. Basic ground-water hydrology [texte imprimé] / Heath, R. C. . - United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1983.
ISSN : CI-05068
Each section consists of a brief text and one or more drawings or maps that illustrate the main points covered in the text. Because the text is, in effect, an expanded discussion of the illustrations, most of the illustrations are not captioned. However, where more than one drawing is included in a section, each drawing is assigned a number, given in parentheses, and these numbers are inserted at places in the text where the reader should refer to the drawing.
Langues : Anglais (eng)
Mots-clés : Eau souterraine Cycle de l'eau Topographie Qualité de l'eau Pollution Température Index. décimale : 551.48 Hydrologie : Résumé : Each section consists of a brief text and one or more drawings or maps that illustrate the main points covered in the text. Because the text is, in effect, an expanded discussion of the illustrations, most of the illustrations are not captioned. However, where more than one drawing is included in a section, each drawing is assigned a number, given in parentheses, and these numbers are inserted at places in the text where the reader should refer to the drawing. Note de contenu : Each section consists of a brief text and one or more drawings or maps that illustrate the main points covered in the text. Because the text is, in effect, an expanded discussion of the illustrations, most of the illustrations are not captioned. However, where more than one drawing is included in a section, each drawing is assigned a number, given in parentheses, and these numbers are inserted at places in the text where the reader should refer to the drawing. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B068.87185 CI-05068 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B068.87186 CI-05068 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B068.87184 CI-05068 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B068.87183 CI-05068 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B068.87182 CI-05068 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B068.87179 CI-05068 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B068.87181 CI-05068 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B068.87180 CI-05068 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible U.S. Geological Survey Water Supply paper, 2221. Hydrology of major estuaries and sounds of north Carolina / Giese, G. L.
Titre de série : U.S. Geological Survey Water Supply paper, 2221 Titre : Hydrology of major estuaries and sounds of north Carolina Type de document : texte imprimé Auteurs : Giese, G. L. ; Wilder, H. B. ; Parker, G. G. Mention d'édition : United States Gouvernment Printing Office Editeur : United States Gouvernment Printing Office Année de publication : 1985 ISBN/ISSN/EAN : CI-05069 Note générale : "This report is divided into four chapters. The first, ""general hydrology"", is primarily a discussion of basic hydrologic principles relating to tides, tidal flow, salinity, sedimentation, and the effects of winds and hurricanes. The other three chapters summarize present knowledge of the hydrology of individual sounds and estuaries in each of three estuarine systems. The estuarine systems are, in oder of discussion, the Cape Fear River system, the Pamlico sound system, and the Albemarle sound system. The comprehensiveness of the summaries for each sound orestamp is directly related to the availability of information on which the summaries are based. The Cape Fear River estuary, for example, has been much more thoroughly studies than the Roanoke river." Langues : Anglais (eng) Mots-clés : Hydrologie Estuaire Sédimentation Eau douce Eau salée Qualité de l'eau Géomorphologie Index. décimale : 551.48 Hydrologie : Résumé : "This report is divided into four chapters. The first, ""general hydrology"", is primarily a discussion of basic hydrologic principles relating to tides, tidal flow, salinity, sedimentation, and the effects of winds and hurricanes. The other three chapters summarize present knowledge of the hydrology of individual sounds and estuaries in each of three estuarine systems. The estuarine systems are, in oder of discussion, the Cape Fear River system, the Pamlico sound system, and the Albemarle sound system. The comprehensiveness of the summaries for each sound orestamp is directly related to the availability of information on which the summaries are based. The Cape Fear River estuary, for example, has been much more thoroughly studies than the Roanoke river." Note de contenu : "This report is divided into four chapters. The first, ""general hydrology"", is primarily a discussion of basic hydrologic principles relating to tides, tidal flow, salinity, sedimentation, and the effects of winds and hurricanes. The other three chapters summarize present knowledge of the hydrology of individual sounds and estuaries in each of three estuarine systems. The estuarine systems are, in oder of discussion, the Cape Fear River system, the Pamlico sound system, and the Albemarle sound system. The comprehensiveness of the summaries for each sound orestamp is directly related to the availability of information on which the summaries are based. The Cape Fear River estuary, for example, has been much more thoroughly studies than the Roanoke river." U.S. Geological Survey Water Supply paper, 2221. Hydrology of major estuaries and sounds of north Carolina [texte imprimé] / Giese, G. L. ; Wilder, H. B. ; Parker, G. G. . - United States Gouvernment Printing Office . - United States Gouvernment Printing Office, 1985.
ISSN : CI-05069
"This report is divided into four chapters. The first, ""general hydrology"", is primarily a discussion of basic hydrologic principles relating to tides, tidal flow, salinity, sedimentation, and the effects of winds and hurricanes. The other three chapters summarize present knowledge of the hydrology of individual sounds and estuaries in each of three estuarine systems. The estuarine systems are, in oder of discussion, the Cape Fear River system, the Pamlico sound system, and the Albemarle sound system. The comprehensiveness of the summaries for each sound orestamp is directly related to the availability of information on which the summaries are based. The Cape Fear River estuary, for example, has been much more thoroughly studies than the Roanoke river."
Langues : Anglais (eng)
Mots-clés : Hydrologie Estuaire Sédimentation Eau douce Eau salée Qualité de l'eau Géomorphologie Index. décimale : 551.48 Hydrologie : Résumé : "This report is divided into four chapters. The first, ""general hydrology"", is primarily a discussion of basic hydrologic principles relating to tides, tidal flow, salinity, sedimentation, and the effects of winds and hurricanes. The other three chapters summarize present knowledge of the hydrology of individual sounds and estuaries in each of three estuarine systems. The estuarine systems are, in oder of discussion, the Cape Fear River system, the Pamlico sound system, and the Albemarle sound system. The comprehensiveness of the summaries for each sound orestamp is directly related to the availability of information on which the summaries are based. The Cape Fear River estuary, for example, has been much more thoroughly studies than the Roanoke river." Note de contenu : "This report is divided into four chapters. The first, ""general hydrology"", is primarily a discussion of basic hydrologic principles relating to tides, tidal flow, salinity, sedimentation, and the effects of winds and hurricanes. The other three chapters summarize present knowledge of the hydrology of individual sounds and estuaries in each of three estuarine systems. The estuarine systems are, in oder of discussion, the Cape Fear River system, the Pamlico sound system, and the Albemarle sound system. The comprehensiveness of the summaries for each sound orestamp is directly related to the availability of information on which the summaries are based. The Cape Fear River estuary, for example, has been much more thoroughly studies than the Roanoke river." Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B069.77738 CI-05069 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B069.77737 CI-05069 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B069.77736 CI-05069 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B069.77735 CI-05069 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B069.77734 CI-05069 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B069.77733 CI-05069 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B069.77732 CI-05069 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B069.77731 CI-05069 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible 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.
PermalinkU.S. Geological Survey Water Supply paper, 2230. A filtration and colum-absorption system for onsite concentration and fractionation of organic substances from large volumes of water / Leenheer, J. A.
PermalinkU.S. Geological Survey Water Supply paper, 2238. Interpolating water-table altitude in west-central Kansas using kriging techniques / Dunlap, L. E.
PermalinkU.S. Geological Survey Water Supply paper, 2243. Changes in flood responses of the Red River of the north basin, north Dakota - Minnesota / MIller, J. E.
PermalinkU.S. Geological Survey Water Supply paper, 2246. Hydrology of the price river basin, Utah with emphasis on select coal-field areas / Waddell, K. M.
PermalinkU.S. Geological Survey Water Supply paper, 2247. Chemical and physical characteristics of water and sediment in scofield reservoir, carbon county, Utah / Waddell, K. M.
PermalinkU.S. Geological Survey Water Supply paper, 2252. Use of the routing procedure to study dye and gas transport in West Fork Trinity river, Texas / Jobson, H. E.
PermalinkU. S. Geological Survey Water Supply paper, 2254. Study and interpretation of the chemical characteristics of natural water / Hem, J. D.
PermalinkU.S. Geological survey water-supply paper, 2256-B. Effects of low level dams on the distribution of sediment trace metals and organic substances in the lower schuylkill river bassin, Pennsylvania / Yorke, T. H.
PermalinkU.S. Geological Survey Water Supply paper, 2256-A. Distribution and transport of trace substances in the Schurylkill River Bassin from Berne to Philadelphia, Pennsylvania / Staner, J. K.
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