109 documents satisfont la requête.
Le rôle des entités sub-étatiques dans les processus d'intégration continentale et sub-continentale : les paramètres de comparaison dans cinq espaces géopolitiques ; Le rôle des entités sub-étatiques dans les processus d'intégration continentale et sub-continentale : les paramètres de comparaison dans cinq espaces géopolitiques
Auteur(s) : Pasquier, Romain Pasquier, Romain Pasquier, Romain
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Quelle promotion pour les entités infra-étatiques dans les organisations d'intégration et de coopération régionales ? : Les enseignements de la politique de cohésion de l'Union européenne
Auteur(s) : Michea, Frédérique
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TIC et processus de démocratisation en Afrique : pour un système de gestion transparente des élections par l'expérience du "Parellel Vote Tabulation" (PVT)
Auteur(s) : Kone, Tahirou
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L'apport de la culture reggae jamaïcaine dans l'élaboration d'une civilisation caribéenne
Auteur(s) : Kroubo-Dagnini, Jérémie
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Example Insert Sheet for Archival Collections, Added to Folders in Archival Collections When Items Are Digitized)
Auteur(s) : Taylor, Laurie N.
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Numerical study of shear on cohesive granular geomaterials : micro-macro relations, microstructure, and application to the simulation of landslides ; Étude numérique du cisaillement des géomatériaux granulaires cohésifs : passage micro-macro, microstructure, et application à la modélisation de glissements de terrain
Auteur(s) : Estrada Mejía, Nicolás
Auteurs secondaires : Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Université Montpellier II - Sciences et Techniques du Languedoc Alfredo Taboada(taboada@gm.univ-montp2.fr)
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Le Fonds structurels de l'UEMOA. Quelle implication des entités infra-étatiques ? ; Le Fonds structurels de l'UEMOA. Quelle implication des entités infra-étatiques ?
Auteur(s) : Ibriga, Luc-Marius Ibriga, Luc-Marius Ibriga, Luc-Marius
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Pourquoi la CTM ? ; Pourquoi la CTM ?
Auteur(s) : François-Lubin, Bertrand François-Lubin, Bertrand
Auteurs secondaires : Lacom, Gérard Lacom, Gérard
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Patrimoine culturel et politique éducative en Guyane
Auteur(s) : Blérald, Monique
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Bals parés-masqués et carnaval en Guyane. La tradition du Randé boutché
Auteur(s) : Pindard, Marie-Françoise
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L’adaptation en zone côtière : de la parole aux actes : études de cas de deux territoires du Sud-Est du Nouveau-Brunswick (Canada) concernant les dynamiques sociales et les apprentissages mutuels de communautés côti
Auteur(s) : Rabeniaina, Tiavina R. Chouinard, Omer Weissenberger, Sebastian
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Flocculation Potential of Estuarine Particles: The Importance of Environmental Factors and of the Spatial and Seasonal Variability of Suspended Particulate Matter
Auteur(s) : Verney, Romaric Lafite, Robert Brun-cottan, Jean-claude
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1,000 A mu m). Flocculation processes were estimated using three parameters: flocculation efficiency, flocculation speed, and flocculation time. Results showed that the flocculation that occurred at the three stations was mainly influenced by the concentration of the suspended particulate matter: maximum floc size was observed for concentrations above 0.1 g l(-1) while no flocculation was observed for concentrations below 0.004 g l(-1). Diatom blooms strongly enhanced flocculation speed and, to a lesser extent, flocculation efficiency. During this period, the maximum flocculation speed of 6 A mu m min(-1) corresponded to a flocculation time of less than 20 min. Salinity did not appear to automatically enhance flocculation, which depended on the constituents of suspended sediments and on the content and concentration of organic matter. Examination of the variability of 2D fractal dimension during flocculation experiments revealed restructuring of flocs during aggregation. This was observed as a rapid decrease in the floc fractal dimension from 2 to 1.4 during the first minutes of the flocculation stage, followed by a slight increase up to 1.8. Deflocculation experiments enabled determination of the influence of turbulent structures on flocculation processes and confirmed that turbulent intensity is one of the main determining factors of maximum floc size."> 1,000 A mu m). Flocculation processes were estimated using three parameters: flocculation efficiency, flocculation speed, and flocculation time. Results showed that the flocculation that occurred at the three stations was mainly influenced by the concentration of the suspended particulate matter: maximum floc size was observed for concentrations above 0.1 g l(-1) while no flocculation was observed for concentrations below 0.004 g l(-1). Diatom blooms strongly enhanced flocculation speed and, to a lesser extent, flocculation efficiency. During this period, the maximum flocculation speed of 6 A mu m min(-1) corresponded to a flocculation time of less than 20 min. Salinity did not appear to automatically enhance flocculation, which depended on the constituents of suspended sediments and on the content and concentration of organic matter. Examination of the variability of 2D fractal dimension during flocculation experiments revealed restructuring of flocs during aggregation. This was observed as a rapid decrease in the floc fractal dimension from 2 to 1.4 during the first minutes of the flocculation stage, followed by a slight increase up to 1.8. Deflocculation experiments enabled determination of the influence of turbulent structures on flocculation processes and confirmed that turbulent intensity is one of the main determining factors of maximum floc size."> 1,000 A mu m). Flocculation processes were estimated using three parameters: flocculation efficiency, flocculation speed, and flocculation time. Results showed that the flocculation that occurred at the three stations was mainly influenced by the concentration of the suspended particulate matter: maximum floc size was observed for concentrations above 0.1 g l(-1) while no flocculation was observed for concentrations below 0.004 g l(-1). Diatom blooms strongly enhanced flocculation speed and, to a lesser extent, flocculation efficiency. During this period, the maximum flocculation speed of 6 A mu m min(-1) corresponded to a flocculation time of less than 20 min. Salinity did not appear to automatically enhance flocculation, which depended on the constituents of suspended sediments and on the content and concentration of organic matter. Examination of the variability of 2D fractal dimension during flocculation experiments revealed restructuring of flocs during aggregation. This was observed as a rapid decrease in the floc fractal dimension from 2 to 1.4 during the first minutes of the flocculation stage, followed by a slight increase up to 1.8. Deflocculation experiments enabled determination of the influence of turbulent structures on flocculation processes and confirmed that turbulent intensity is one of the main determining factors of maximum floc size."> 1,000 A mu m). Flocculation processes were estimated using three parameters: flocculation efficiency, flocculation speed, and flocculation time. Results showed that the flocculation that occurred at the three stations was mainly influenced by the concentration of the suspended particulate matter: maximum floc size was observed for concentrations above 0.1 g l(-1) while no flocculation was observed for concentrations below 0.004 g l(-1). Diatom blooms strongly enhanced flocculation speed and, to a lesser extent, flocculation efficiency. During this period, the maximum flocculation speed of 6 A mu m min(-1) corresponded to a flocculation time of less than 20 min. Salinity did not appear to automatically enhance flocculation, which depended on the constituents of suspended sediments and on the content and concentration of organic matter. Examination of the variability of 2D fractal dimension during flocculation experiments revealed restructuring of flocs during aggregation. This was observed as a rapid decrease in the floc fractal dimension from 2 to 1.4 during the first minutes of the flocculation stage, followed by a slight increase up to 1.8. Deflocculation experiments enabled determination of the influence of turbulent structures on flocculation processes and confirmed that turbulent intensity is one of the main determining factors of maximum floc size."> | 1,000 A mu m). Flocculation processes were estimated using three parameters: flocculation efficiency, flocculation speed, and flocculation time. Results showed that the flocculation that occurred at the three stations was mainly influenced by the concentration of the suspended particulate matter: maximum floc size was observed for concentrations above 0.1 g l(-1) while no flocculation was observed for concentrations below 0.004 g l(-1). Diatom blooms strongly enhanced flocculation speed and, to a lesser extent, flocculation efficiency. During this period, the maximum flocculation speed of 6 A mu m min(-1) corresponded to a flocculation time of less than 20 min. Salinity did not appear to automatically enhance flocculation, which depended on the constituents of suspended sediments and on the content and concentration of organic matter. Examination of the variability of 2D fractal dimension during flocculation experiments revealed restructuring of flocs during aggregation. This was observed as a rapid decrease in the floc fractal dimension from 2 to 1.4 during the first minutes of the flocculation stage, followed by a slight increase up to 1.8. Deflocculation experiments enabled determination of the influence of turbulent structures on flocculation processes and confirmed that turbulent intensity is one of the main determining factors of maximum floc size.">Plus
L'expérience des politiques de l'Union européenne : Débats 04 ; L'expérience des politiques de l'Union européenne : Débats 04
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Diagnostic Study for the DIPECHO Action Plan for Central America and the Caribbean ; Diagnóstico previo al Plan de Acción para América Central y El Caribe ; Diagnostic préalable aux plans d'action DIPECHO en Amérique Centrale et dans les Caraïbes
Auteur(s) : D'Ercole, Robert Lesales, Thierry Pigeon, Patrick Misson, Claudine Napias, Jean-Claude Giri, Jacques Orlyk, Sylvie
Auteurs secondaires : Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]) Université des Antilles et de la Guyane (UAG) Centre de Recherche sur l’Épidémiologie des Désastres - CRED CIFEG ECHO CIFEG (Centre International pour la Formation et les Echanges Géologiques) Programme ECHO de prévention d'atténuation et de préparation aux catastrophes
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Rock-and-soil avalanches: Theory and simulation
Auteur(s) : Taboada, Alfredo Estrada, Nicolas
Auteurs secondaires : Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)
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L’engouement des communautés indigènes équatoriennes pour le tourisme, choix pertinent ou désillusion annoncée ?
Auteur(s) : Schéou, Bernard
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Site mathématique d’une ROC : une nouvelle façon d’interroger un exercice ?
Auteur(s) : Delcroix, Antoine Silvy, Christian
Auteurs secondaires : Centre de recherches et de ressources en éducation et formation (CRREF) ; Université des Antilles et de la Guyane (UAG)
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Fertilité et insuffisance ovarienne : de nouveaux traitements en perspective ? [Ovarian failure: New treatments in perspective?]
Auteur(s) : Ravel, C. Kazdar, N. Leveque, J
Auteurs secondaires : Institut de recherche, santé, environnement et travail [Rennes] (Irset) ; Université d'Angers (UA) - Université des Antilles et de la Guyane (UAG) - Université de Rennes 1 (UR1) - École des Hautes Études en Santé Publique [EHESP] (EHESP) - Institut National de la Santé et de la Recherche Médicale (INSERM) - Structure Fédérative de Recherche en Biologie et Santé de Rennes ( Biosit : Biologie - Santé - Innovation Technologique ) CHU Pontchaillou [Rennes]
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A multidating approach applied to historical slackwater flood deposits of the Gardon River, SE France
Auteur(s) : Dezileau, L. Terrier, B. Berger, J.F. Blanchemanche, P. Latapie, A. Freydier, R. Bremond, L. Paquier, A.
Auteurs secondaires : Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Agence de l'eau Rhône Méditérranée et Corse ; Agence de l'eau Rhône Méditérranée et Corse Environnement Ville Société (EVS) ; Centre National de la Recherche Scientifique (CNRS) - École nationale supérieure d'architecture de Lyon (ENSAL) - Ecole Nationale Supérieure des Mines de Saint-Etienne - École Nationale des Travaux Publics de l'État (ENTPE) - Université Jean Monnet [Saint-Étienne] (UJM) - Université Jean Moulin - Lyon III - Université Lumière - Lyon 2 (UL2) - École normale supérieure - Lyon (ENS Lyon) Archéologie des Sociétés Méditerranéennes (ASM) ; Centre National de la Recherche Scientifique (CNRS) - Université Paul-Valéry - Montpellier 3 (UM3) - Ministère de la Culture et de la Communication (MCC) Hydrologie-Hydraulique (UR HHLY) ; Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA) Hydrosciences Montpellier (HSM) ; Institut de Recherche pour le Développement (IRD) - Université Montpellier 2 - Sciences et Techniques (UM2) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Centre de Bio-Archéologie et d'Ecologie (CBAE) ; Université Montpellier 2 - Sciences et Techniques (UM2) - École pratique des hautes études (EPHE) - Centre National de la Recherche Scientifique (CNRS) Centre d'Etudes et d'Expertise sur les Risques, l'Environnement, la Mobilité et l'Aménagement - Direction Méditerranée (Cerema Direction Méditerranée) ; Centre d'Etudes et d'Expertise sur les Risques, l'Environnement, la Mobilité et l'Aménagement (Cerema)
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“All the world's a stage”: Creating Guanajuato, Mexico’s Tourism Image
Auteur(s) : Asch, Claudia
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