21 documents satisfont la requête.
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
Partager

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
Probiotic effect of FLOC on Vibrios in the pacific white shrimp Litopenaeus Vannamei
Auteur(s) : Aguilera-rivera, Diana Prieto-davo, Alejandra Escalante, Karla Chavez, Cristina Cuzon, Gerard Gaxiola, Gabriela
Partager

| Plus
Morphological Response of a Macrotidal Embayed Beach, Porsmilin, France
Auteur(s) : Floc'h, France Le Dantec, Nicolas Lemos, Clara Cancouët, Romain Sous, Damien Petitjean, Lise Bouchette, Frédéric Ardhuin, Fabrice
Auteurs secondaires : Domaines Océaniques (LDO) ; Centre National de la Recherche Scientifique (CNRS) - Institut d'écologie et environnement - Observatoire des Sciences de l'Univers - Université de Brest (UBO) - Institut national des sciences de l'Univers (INSU - CNRS) Centre d'Etudes et d'Expertise sur les Risques, l'Environnement, la Mobilité et l'Aménagement (Cerema) Littoral, Environnement, Télédétection, Géomatique (LETG - Brest) ; Université de Brest (UBO) - Université d'Angers (UA) - Université de Nantes (UN) - Université de Rennes 2 (UR2) - Institut Universitaire Européen de la Mer (IUEM) ; Institut de Recherche pour le Développement (IRD) - Université de Brest (UBO) - Centre National de la Recherche Scientifique (CNRS) - Institut de Recherche pour le Développement (IRD) - Centre National de la Recherche Scientifique (CNRS) - Centre National de la Recherche Scientifique (CNRS) - Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) Institut méditerranéen d'océanologie (MIO) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Institut de recherche pour le développement [IRD] : UMR235 - Université de Toulon (UTLN) - Centre National de la Recherche Scientifique (CNRS) 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) Laboratoire d'Océanographie Spatiale (LOS) ; Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER) University of Sydney Ana Vila-Concejo, Eleanor Bruce, David M. Kennedy, R. Jack McCarroll
Partager

| Plus
Flora brasiliensis. Volumen X
Auteur(s) : Martius, Carl Friedrich Philipp von (1794-1868)
Année de publication :

Partager

| Plus
DYNALIT : Dynamique du Littoral et Traitde Côte
Auteur(s) : Cocquempot, Lucie Balzer, agnès Bouchette, Frederic Castelle, Bruno Chaumillon, Eric Delacourt, Christophe Duperret, Anne Floc'h, France
Auteurs secondaires : Domaines Océaniques (LDO) ; Centre National de la Recherche Scientifique (CNRS) - Institut d'écologie et environnement - Observatoire des Sciences de l'Univers - Université de Brest (UBO) - Institut national des sciences de l'Univers (INSU - CNRS) Littoral, Environnement, Télédétection, Géomatique (LETG - Nantes) ; Littoral, Environnement, Télédétection, Géomatique (LETG) ; Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) - Université d'Angers (UA) - Université de Nantes (UN) - École pratique des hautes études (EPHE) - Université de Brest (UBO) - Université de Rennes 2 (UR2) - Centre National de la Recherche Scientifique (CNRS) - Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) - Université d'Angers (UA) - Université de Nantes (UN) - École pratique des hautes études (EPHE) - Université de Brest (UBO) - Université de Rennes 2 (UR2) - Centre National de la Recherche Scientifique (CNRS) 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) LIttoral ENvironnement et Sociétés - UMR 7266 (LIENSs) ; Université de La Rochelle (ULR) - Centre National de la Recherche Scientifique (CNRS) Littoral, Environnement, Télédétection, Géomatique (LETG - Caen) ; Littoral, Environnement, Télédétection, Géomatique (LETG) ; Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) - Université d'Angers (UA) - Université de Nantes (UN) - École pratique des hautes études (EPHE) - Université de Brest (UBO) - Université de Rennes 2 (UR2) - Centre National de la Recherche Scientifique (CNRS) - Université de Caen Normandie (UNICAEN) ; Normandie Université (NU) - Normandie Université (NU) - Université d'Angers (UA) - Université de Nantes (UN) - École pratique des hautes études (EPHE) - Université de Brest (UBO) - Université de Rennes 2 (UR2) - Centre National de la Recherche Scientifique (CNRS) Laboratoire Ondes et Milieux Complexes (LOMC) ; Université Le Havre Normandie (ULH) ; Normandie Université (NU) - Normandie Université (NU) - Centre National de la Recherche Scientifique (CNRS) Laboratoire d’Océanologie et de Géosciences (LOG) - UMR 8187 (LOG) ; Centre National de la Recherche Scientifique (CNRS) - Université du Littoral Côte d'Opale - Université de Lille, Sciences et Technologies Morphodynamique Continentale et Côtière (M2C) ; Centre National de la Recherche Scientifique (CNRS) - Université de Rouen Normandie (URN) ; Normandie Université (NU) - Normandie Université (NU) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Caen Normandie (UNICAEN) ; Normandie Université (NU)
Partager

| Plus
Analyzing the market position of fish species subject to the impact of long-term changes: a case study of French fisheries in the Bay of Biscay
Auteur(s) : Le Floc' H, P Poulard, Jean-charles Thebaud, Olivier Blanchard, Fabian Bihel, J Steinmetz, Fabien
Partager

| Plus
Colonization of coastal environments by foraminifera: insight from shrimp ponds in New Caledonia (sw Pacific)
Auteur(s) : Debenay, J. -p. Della Patrona, Luc Goguenheim, H.
Partager

| Plus
A bio-economic analysis of long term changes in the production of French fishing fleets operating in the Bay of Biscay
Auteur(s) : Steinmetz, Fabien Thebaud, Olivier Blanchard, Fabian Le Floc H, Pascal Bihel, J
Partager

| Plus
La France et ses colonies. Tome 1: En France
Auteur(s) : Reclus, Onésime (1837-1916)
Année de publication :

Partager

| Plus
Flora brasiliensis. Volumen IV. Pars I
Auteur(s) : Martius, Carl Friedrich Philipp von (1794-1868)
Année de publication :

Partager

| Plus
Cristalline Boisnoir ou les dangers du bal loulou
Auteur(s) : Herpin, Thérèse
Année de publication :

Partager

| Plus
Les colonies pendant la Révolution : la Constituante et la réforme coloniale
Auteur(s) : Deschamps, Léon (1849-19..)
Année de publication :

Partager

| Plus
De la pétition des ouvriers pour l'abolition immédiate de l'esclavage
Auteur(s) : Schoelcher, Victor (1804-1893)
Année de publication :

Partager

| Plus
Vites boreali americanæ : mémoire
Auteur(s) : Durand, Elias (1794-1873)
Auteurs secondaires : Des Moulins, Charles (1798-1876)
Année de publication :

Partager

| Plus
Sur la piste de l'or : reportage
Auteur(s) : Faugier, Stéphane
Année de publication :

Partager

| Plus