193 documents satisfont la requête.
Forum with Parliament Members : Students Against Sexual Orientation Discrimination ; Audio Recordings of the Proceedings
Auteur(s) : Caribbean IRN
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La promesse post-raciale dans l'Amérique d'Obama ; La promesse post-raciale dans l'Amérique d'Obama
Auteur(s) : Boisseron, Bénédicte Boisseron, Bénédicte
Année de publication :

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Sources and Fate of Organic Matter in Ocean Sediments
Auteur(s) : Tissot, B Pelet, R
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Everald Brown with a religious themed painting ; The Bryant Slides Collection ; The Bryant Slides Collection, Jamaica
Auteur(s) : Unknown ( Photographer ) Brown, Everald, 1917-2002 ( Artist )
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Land Exploitative Activities and Economic Patterns in a Barbados Village
Auteur(s) : Handler, Jerome S.
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Origine de la sédimentation dans le delta de l'Orénoque et le golfe de Paria (Venezuela) : impact du système dispersif amazonien
Auteur(s) : Pujos, M Monente, J Latouche, C Maillet, N
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The stranger in the tropics
Auteur(s) : Tyng, C. D Jay I. Kislak Collection (Library of Congress)
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Paintings on the wall of Everald Brown's studio ; The Bryant Slides Collection ; The Bryant Slides Collection, Jamaica
Auteur(s) : Brown, Everald, 1917-2002 ( Artist ) Unknown ( Photographer )
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British Guiana 1898 : Punishment for Sodomy meted out to Nabi Baksh and Mohangoo on the Mersey ; Report from the Governor to the Colonial Office
Auteur(s) : Walter Sendall Governor of British Guiana
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El petróleo y su incidencia en la economía y el desarrollo de la República Dominicana
Auteur(s) : Fernández, Leonel Rodríguez Padilla, Víctor Orozco, María del Carmen Emam-Zadé, Frederic Despradel, Carlos, 1942- Santana, Isidoro Guzmán, Rolando Alarcón, Rolfi
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Everald Brown and three of his children playing instruments in his studio ; The Bryant Slides Collection ; The Bryant Slides Collection, Jamaica
Auteur(s) : Unknown ( Photographer ) Brown, Everald, 1917-2002
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Bulletin du canal interocéanique ; Canal interocéanique
Auteur(s) : Compagnie universelle du canal interocéanique de Panama
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Report of the Lords of the Committee of Council Appointed for the Consideration of All Matters Relating to Trade And Foreign Plantations: Submitting to His Majesty's Consideration the Evidence And Information They Have Collected In Consequence of His Majesty's Order In Council, Dated the 11th of February 1788, Concerning the Present State of the Trade to Africa, And Particularly the Trade In Slaves; And Concerning the Effects And Consequences of This Trade, As Well In Africa And the West Indies, As to the General Commerce of This Kingdom
Auteur(s) : Great Britain. Board of Trade.
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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
The gem of the Caribbean
Auteur(s) : Wright, Irene Aloha, 1879-1972
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Direct DOC and nitrate determination in water using dual pathlength and second derivative UV spectrophotometry
Auteur(s) : Causse, Jean Thomas, Olivier Jung, Aude-Valérie Thomas, Marie-Florence
Auteurs secondaires : École des Hautes Études en Santé Publique [EHESP] (EHESP) 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 ) Ecole des Métiers de l'Environnement (EME) ; Ecole des Métiers de l'Environnement Association Nationale de la Recherche et de la Technologie (ANRT) Coop de France Ouest Agence de l'Eau Loire-Bretagne Conseil Regional de Bretagne
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Molecular evidence for recent land use change from a swampy environment to a pond (Lorraine, France)
Auteur(s) : Bertrand, O. Mansuy-Huault, L. Montarges-Pelletier, E. Losson, B. Argant, J. Ruffaldi, P. Etienne, D. Garnier, E.
Auteurs secondaires : Géologie et gestion des ressources minérales et énergétiques (G2R) ; Université Henri Poincaré - Nancy 1 (UHP) - Institut National Polytechnique de Lorraine (INPL) - Centre de recherches sur la géologie des matières premières minérales et énergétiques (CREGU) - Centre National de la Recherche Scientifique (CNRS) Laboratoire Environnement et Minéralurgie (LEM) ; Institut National Polytechnique de Lorraine (INPL) - Centre National de la Recherche Scientifique (CNRS) Laboratoire méditerranéen de préhistoire Europe-Afrique (LAMPEA) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Ministère de la Culture et de la Communication (MCC) - Institut national de recherches archéologiques préventives (Inrap) - Centre National de la Recherche Scientifique (CNRS) Laboratoire Chrono-environnement (LCE) ; Université Bourgogne Franche-Comté (UBFC) - Centre National de la Recherche Scientifique (CNRS) - Université de Franche-Comté (UFC) Centre de recherche d'histoire quantitative (CRHQ) ; Centre National de la Recherche Scientifique (CNRS) - Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) Risques ; 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 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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Étude des déterminants géographiques et spatialisation des stocks de carbone des sols de la Martinique
Auteur(s) : Venkatapen, Corinne
Auteurs secondaires : Antilles-Guyane Dolique, Franck Blanchard, Éric
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Are algae relevant to the detritus-based food web in tank-bromeliads?
Auteur(s) : Brouard, Olivier Le Jeune, Anne-Hélène Leroy, Céline Cereghino, Régis Roux, Olivier Pelozuelo, Laurent Dejean, Alain Corbara, Bruno
Auteurs secondaires : Laboratoire Microorganismes : Génome et Environnement (LMGE) ; Université Blaise Pascal - Clermont-Ferrand 2 (UBP) - Université d'Auvergne - Clermont-Ferrand I (UdA) - Centre National de la Recherche Scientifique (CNRS) Ecologie des forêts de Guyane (ECOFOG) ; Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) - Institut National de la Recherche Agronomique (INRA) - Université des Antilles et de la Guyane (UAG) - AgroParisTech - Centre National de la Recherche Scientifique (CNRS) Laboratoire Ecologie Fonctionnelle et Environnement - ECOLAB (ECOLAB) ; Institut National Polytechnique [Toulouse] (INP) - Université Paul Sabatier - Toulouse 3 (UPS) - Observatoire Midi-Pyrénées (OMP) - Centre National de la Recherche Scientifique (CNRS) Université Paul Sabatier - Toulouse 3 (UPS)
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Les apports organiques et leur transformation en milieu abyssal à l'interface eau-sédiment dans l'Océan Atlantique tropical
Auteur(s) : Khripounoff, Alexis Rowe, Gilbert T
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