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HYDROLOGICAL PROCESSES AND WATER MANAGEMENT IN … HYDROLOGICAL PROCESSES AND WATER MANAGEMENT IN URBAN AREAS Edited by Herbert MASSING Landesamt fur Wasser und Abfall Noidrhein-Westfalen,P.O. Box 5227,
GROUNDWATER TRACING
Groundwater tracing 121 Intentional labelling by means of noble gases has been used only in surface waters for measurements of gas exchange with the atmosphere.DROUGHTS AND FLOODS
317 Droughts and floods — their definition and modeling or median value of annual maxima: Qf = i 2 Q™7 . , (7) cfc = Q (8) In the next section of this paper some other values of Qf for hydrolo- gical criteria are discussed, with the requirements of statistical ana RADIONUCLIDES IN GROUNDWATERS: CONTAMINANTS AND TRACERS Radionuclides in groundwaters: contaminants and tracers 5 A, = Ae (1) where A, is the activity of the daughter nuclide at time t (here assumed to be residence time (Bq l"1)), A e is the activity of daughter nuclide at secular equilibrium with parent nuclide, (Bq l"1), and X is the radioactive decay constant of daughter (X = ri/2/ln2; Tm= half life) (f1).
SINGLE-PARAMETER SENSITIVITY ANALYSIS FOR AQUIFER Single-parameter sensitivity analysis using DRASTIC and SINTACS 561 METHOD IMPLEMENTATION The procedure developed to perform the sensitivity analysis is shown in Fig. 1 and is ESTIMATION OF THE SUSTAINABLE YIELD OF A BOREHOLE 368 Gerritt van Tonder et al. storativity S. If ti ong describes the maximum operation time in which the drawdown s shall not exceed a maximum drawdown s Available, the extrapolation of the measured pumping test drawdown can be used to determine the sustainable yield Qsustamabie- ^ Available tiSustainable *lPump Test (f — f \ S Pump Test V' — ' long ) The available drawdown is for instance HIGHEST FLOODS IN INDIA 168 P. R. Rakhecha Fig. 1 Major river basins of India and locations of the highest floods in India. the Brahamaputra River are the important Himalayan rivers in the northern part of India. These rivers are both snowfed and rainfed and therefore have continuous flow HYDROLOGICAL DATA COLLECTION, INTERPRETATION AND ANALYSIS Hydrologie Applications of Space Technology (Proceedings of the Cocoa Beach Workshop, Florida, August 1985). IAHS Publ. no. 160, 1986. Hydrological data collection, interpretation WORLD WATER BALANCE (GENERAL REPORT) World Water Balunce World water balance (General report) Professor M. I. Lvovitch, Institute of Geography of the AS of the USSR, Moscow RESUME : Cette communicatjon expose la notion de bilan hydrique mondial en général, ainsi que l'importance qu'elle revêt notamment pour accroître notre connaissance des processus hydrolo- ESTIMATION DES VALEURS EXTRÊMES DE DÉBIT PAR LA MÉTHODE SHYREG Université Pierre et Marie Curie, École Doctorale 389 Géosciences et Ressources Naturelles Thèse de doctorat Estimation des valeursextrêmes
HYDROLOGICAL PROCESSES AND WATER MANAGEMENT IN … HYDROLOGICAL PROCESSES AND WATER MANAGEMENT IN URBAN AREAS Edited by Herbert MASSING Landesamt fur Wasser und Abfall Noidrhein-Westfalen,P.O. Box 5227,
GROUNDWATER TRACING
Groundwater tracing 121 Intentional labelling by means of noble gases has been used only in surface waters for measurements of gas exchange with the atmosphere.DROUGHTS AND FLOODS
317 Droughts and floods — their definition and modeling or median value of annual maxima: Qf = i 2 Q™7 . , (7) cfc = Q (8) In the next section of this paper some other values of Qf for hydrolo- gical criteria are discussed, with the requirements of statistical ana RADIONUCLIDES IN GROUNDWATERS: CONTAMINANTS AND TRACERS Radionuclides in groundwaters: contaminants and tracers 5 A, = Ae (1) where A, is the activity of the daughter nuclide at time t (here assumed to be residence time (Bq l"1)), A e is the activity of daughter nuclide at secular equilibrium with parent nuclide, (Bq l"1), and X is the radioactive decay constant of daughter (X = ri/2/ln2; Tm= half life) (f1).
SINGLE-PARAMETER SENSITIVITY ANALYSIS FOR AQUIFER Single-parameter sensitivity analysis using DRASTIC and SINTACS 561 METHOD IMPLEMENTATION The procedure developed to perform the sensitivity analysis is shown in Fig. 1 and is ESTIMATION OF THE SUSTAINABLE YIELD OF A BOREHOLE 368 Gerritt van Tonder et al. storativity S. If ti ong describes the maximum operation time in which the drawdown s shall not exceed a maximum drawdown s Available, the extrapolation of the measured pumping test drawdown can be used to determine the sustainable yield Qsustamabie- ^ Available tiSustainable *lPump Test (f — f \ S Pump Test V' — ' long ) The available drawdown is for instance HIGHEST FLOODS IN INDIA 168 P. R. Rakhecha Fig. 1 Major river basins of India and locations of the highest floods in India. the Brahamaputra River are the important Himalayan rivers in the northern part of India. These rivers are both snowfed and rainfed and therefore have continuous flow 0360EN - HYDROLOGIE.ORG 0360EN. EN 0360 drainage basin syn. catchment; catchment area; drainage area; river basin; watershed (AU); see also basin ; Area having a common outlet for its surface runoff. (TR) Vide. 1317EN - HYDROLOGIE.ORG 1317EN. EN 1317 unconfined aquifer syn. free aquifer; water table aquifer; Aquifer containing unconfined groundwater, that is having a water table and an unsaturated zone. Vide.JOURNAL
Volume 43, Number 6, December 1998 HYDROLOGICAL SCIENCES JOURNAL DES SCIENCES HYDROLOGIQUES Editor: Zbigniew W. Kundzewicz c/o IAHS Press, Institute of Hydrology, Wallingford, Oxfordshire OX10 8BB, UK PATHOLOGIES, IMPROVEMENTS AND OPTIMISM Hydrological Sciences–Journal–des Sciences Hydrologiques, 51(2) April 2006 357 Pathologies, improvements and optimism Reply to discussions of “Editorial—The peer review system: prospects CONCEPTS OF THE HYDROLOGICAL CYCLE Colloque International OH2 « Origines et Histoire de l’Hydrologie », Dijon, 9-11 mai 2001 International Symposium OH2 ‘Origins and History of Hydrology’, Dijon, May, 9-11, 2001HYDROLOGIE.ORG
Author: KONICA MINOLTA 920 Created Date: 6/26/2008 8:23:39 PM WETLAND AND RIVER FLOW INTERACTIONS IN ZIMBABWE Wetland and river flow interactions in Zimbabwe 307 objective of this paper to examine the origins of the concept of river flow maintenance by dambos in Zimbabwe, in the context of hydrological knowledgerelating to dambos
MAJOR, MINOR, AND TRACE ELEMENT CHEMISTRY OF SURFACE Biogeochemistry of Seasonally Snow-Covered Catchments (Proceedings of a Boulder Symposium July 1995). IAHS Publ. no. 228, 1995. 405 Major, minor, and trace element chemistry of surfaceHYDROLOGIE.ORG
Hydrologie.org
LATERAL VARIABILITY OF OVERBANK SEDIMENTATION ON A DEVON Lateral variability of overbank sedimentation on a Devon flood plain 717 THE STUDY SITE The River Culm (Fig. 1), a tributary of the River Exe in southeast Devon, was HYDROLOGIE.ORGTRANSLATE THIS PAGE HYDROLOGIE.ORG. Pierre Hubert, fondateur et concepteur de ce site, est décédé le 31 décembre dernier à Paris. Tous témoignent de son humanité, de sa vitalité joyeuse, et de son énergie sans faille à rassembler et faire connaître l'hydrologie et les hydrologues dumonde entier.
GROUNDWATER TRACING
Groundwater tracing 121 Intentional labelling by means of noble gases has been used only in surface waters for measurements of gas exchange with the atmosphere. ESTIMATION DES VALEURS EXTRÊMES DE DÉBIT PAR LA MÉTHODE SHYREG Université Pierre et Marie Curie, École Doctorale 389 Géosciences et Ressources Naturelles Thèse de doctorat Estimation des valeursextrêmes
TEMPS DE RETOUR
Commentaires: - La notion de temps de retour est destinée à caractériser la fréquence d’apparition d'un phénomène. C'est sans doute dans un souci pédagogique que les statisticiens ont voulu traduire la probabilité d'un évènement, notion réputée particulièrement absconse, en temps de retour, supposé plus compréhensible pour les responsables et le grand public. RADIONUCLIDES IN GROUNDWATERS: CONTAMINANTS AND TRACERS Radionuclides in groundwaters: contaminants and tracers 5 A, = Ae (1) where A, is the activity of the daughter nuclide at time t (here assumed to be residence time (Bq l"1)), A e is the activity of daughter nuclide at secular equilibrium with parent nuclide, (Bq l"1), and X is the radioactive decay constant of daughter (X = ri/2/ln2; Tm= half life) (f1).
NAPPE D'ACCOMPAGNEMENTTRANSLATE THIS PAGE Référence: Décret n° 93.743 du 29 mars 1993 (en application de la Loi sur l'eau du 3 janvier 1992).Collin et Daum, 1996. Remarque: Le texte réglementaire cité ne donne pas de définition du terme nappe d'accompagnement introduit. HEAT TRANSFER COEFFICIENTS FOR NATURAL WATER SURFACES wave radiation. The heat loss by convection is proportional to h (T0 — Ta), where T0 and Ta are the temperatures of the body and the air surrounding the body, and /; is a coefficient which will vary with the shape and dimensions of the surface and the ESTIMATION OF THE SUSTAINABLE YIELD OF A BOREHOLE 368 Gerritt van Tonder et al. storativity S. If ti ong describes the maximum operation time in which the drawdown s shall not exceed a maximum drawdown s Available, the extrapolation of the measured pumping test drawdown can be used to determine the sustainable yield Qsustamabie- ^ Available tiSustainable *lPump Test (f — f \ S Pump Test V' — ' long ) The available drawdown is for instance OBJECTIVES AND PREVENTION METHODS FOR GLACIER LAKE Snow and Glacier Hydrology (Proceedings of the Kathmandu Symposium, November 1992). IAHS Publ. no. 218,1993. 341 Objectives and PreventionMethods for Glacier
REMOTE SENSING APPLICATIONS IN AFRICAN EROSION AND Remote sensing and erosion and sedimentation 377 imagery since its availability is dependent on high-cost project specific monitoring events, but with the launch of ERS-1 in 1988 HYDROLOGIE.ORGTRANSLATE THIS PAGE HYDROLOGIE.ORG. Pierre Hubert, fondateur et concepteur de ce site, est décédé le 31 décembre dernier à Paris. Tous témoignent de son humanité, de sa vitalité joyeuse, et de son énergie sans faille à rassembler et faire connaître l'hydrologie et les hydrologues dumonde entier.
GROUNDWATER TRACING
Groundwater tracing 121 Intentional labelling by means of noble gases has been used only in surface waters for measurements of gas exchange with the atmosphere. ESTIMATION DES VALEURS EXTRÊMES DE DÉBIT PAR LA MÉTHODE SHYREG Université Pierre et Marie Curie, École Doctorale 389 Géosciences et Ressources Naturelles Thèse de doctorat Estimation des valeursextrêmes
TEMPS DE RETOUR
Commentaires: - La notion de temps de retour est destinée à caractériser la fréquence d’apparition d'un phénomène. C'est sans doute dans un souci pédagogique que les statisticiens ont voulu traduire la probabilité d'un évènement, notion réputée particulièrement absconse, en temps de retour, supposé plus compréhensible pour les responsables et le grand public. RADIONUCLIDES IN GROUNDWATERS: CONTAMINANTS AND TRACERS Radionuclides in groundwaters: contaminants and tracers 5 A, = Ae (1) where A, is the activity of the daughter nuclide at time t (here assumed to be residence time (Bq l"1)), A e is the activity of daughter nuclide at secular equilibrium with parent nuclide, (Bq l"1), and X is the radioactive decay constant of daughter (X = ri/2/ln2; Tm= half life) (f1).
NAPPE D'ACCOMPAGNEMENTTRANSLATE THIS PAGE Référence: Décret n° 93.743 du 29 mars 1993 (en application de la Loi sur l'eau du 3 janvier 1992).Collin et Daum, 1996. Remarque: Le texte réglementaire cité ne donne pas de définition du terme nappe d'accompagnement introduit. HEAT TRANSFER COEFFICIENTS FOR NATURAL WATER SURFACES wave radiation. The heat loss by convection is proportional to h (T0 — Ta), where T0 and Ta are the temperatures of the body and the air surrounding the body, and /; is a coefficient which will vary with the shape and dimensions of the surface and the ESTIMATION OF THE SUSTAINABLE YIELD OF A BOREHOLE 368 Gerritt van Tonder et al. storativity S. If ti ong describes the maximum operation time in which the drawdown s shall not exceed a maximum drawdown s Available, the extrapolation of the measured pumping test drawdown can be used to determine the sustainable yield Qsustamabie- ^ Available tiSustainable *lPump Test (f — f \ S Pump Test V' — ' long ) The available drawdown is for instance OBJECTIVES AND PREVENTION METHODS FOR GLACIER LAKE Snow and Glacier Hydrology (Proceedings of the Kathmandu Symposium, November 1992). IAHS Publ. no. 218,1993. 341 Objectives and PreventionMethods for Glacier
REMOTE SENSING APPLICATIONS IN AFRICAN EROSION AND Remote sensing and erosion and sedimentation 377 imagery since its availability is dependent on high-cost project specific monitoring events, but with the launch of ERS-1 in 1988HYDROSYSTEME
Définitions existantes. A noter que le terme hydrosystème ne figure ni dans le Larousse, ni dans le Robert, ni dans le Trésor de la Langue Française.. Le Dictionnaire français d'hydrologie de surface (M. Roche, 1986) donne la définition suivante pour système d'eau: "tout ensemble hydrologique comportant ou non des aménagements : le réseau hydrographique d'un bassin en est un exemple. HYDROLABTRANSLATE THIS PAGE Logiciel développé par J.P. Laborde, Professeur à l'Université de Nice - Sophia Antipolis, assisté de N. Mouhous. UMR 5651 "espace" du CNRS, Université de Nice - Sophia Antipolis. 98 Bd E. Herriot, BP 209, 06204 Nice Cedex 3, France. Courriel : laborde@unice.fr. Manuel d'utilisation du logiciel HYDROLAB. Notice d'installation du logiciel 0360EN - HYDROLOGIE.ORG 0360EN. EN 0360 drainage basin syn. catchment; catchment area; drainage area; river basin; watershed (AU); see also basin ; Area having a common outlet for its surface runoff. (TR) Vide. HYDROLOGIE.ORGTRANSLATE THIS PAGEHydrologie.org
BILAN HYDRIQUE
Définition proposée. Dans tous les cas c'est l'aspect comptable du terme bilan qui prévaut en hydrologie, que ce soit au niveau des bilans hydriques ou hydrologiques. Trop souvent confondus, ces deux termes sont bien replacés dans leurs domaines respectifs par le Larousse Encyclopédique : le bilan hydrologique se situe à l'échelle du bassin versant et concerne une démarche hydrologiqueHYDROLOGIE.ORG
Author: KONICA MINOLTA 920 Created Date: 6/26/2008 8:23:39 PM SURFACE, VOLUME ET PROFONDEUR MOYENNE DES MERS …TRANSLATE THIS PAGE Surface, volume et profondeur moyenne des mers et océans. Surface, volume et profondeur moyenne des mers et océans. (Kossinna, 1921) Surface. 10**6 km². Volume. 10**6 km³. Prof. moy. 1231ZH - HYDROLOGIE.ORG 1231ZH - hydrologie.org FRAME-INDEX-ESTRANSLATE THIS PAGE capa semiconfinada. capacidad. capacidad (humedad) de retención capilar. capacidad calorÃfica. capacidad de absorción. capacidad de aliviadero. capacidad de almacenamiento anual. capacidad de almacenamiento interanual. capacidad de arrastre de sedimentos. MEMOIRE POUR L’OBTENTION DU MASTER EN INGENIERIE DE … Mémoire de fin d’étude : Contribution à la révision des normes hydrologiques au Burkina Faso Année 2010/2011 ~ iii ~ BAMBARA Télado Luc REMERCIEMENTS Je remercie l’ensemble desHYDROLOGIE.ORG
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