392 documents satisfont la requête.
Recueil de législation, de doctrine et de jurisprudence coloniales. Tome 39
Année de publication :

Partager

| Plus
Traité de droit colonial. Tome II
Auteur(s) : Dareste de La Chavanne, Pierre-Rodolphe (1851-1937)
Auteurs secondaires : Matter, Paul (1865-1938)
Année de publication :

Partager

| Plus
Bulletin officiel de la Guyane française
Année de publication :

Partager

| Plus
Les colonies françaises : un siècle d'expansion coloniale
Auteur(s) : Terrier, Auguste (1873-1932) Dubois, Marcel (1856-1916)
Auteurs secondaires : France. Ministère des colonies (1894-1946)
Année de publication :

Partager

| Plus
Voyage pittoresque dans les deux Amériques : résumé général de tous les voyages…
Auteur(s) : Orbigny, Alcide d' (1802-1857)
Auteurs secondaires : Sainson
Année de publication :

Partager

| Plus
Lettres édifiantes et curieuses, écrites des missions étrangères. Tome huitième, Mémoires d'amérique
Année de publication :

Partager

| Plus
Biologie et peche du capitaine Lethrinus enigmaticus (Smith) 1959 du banc de Saya de Malha (Ocean Indien)
Auteur(s) : Lebeau, A Cueff, J.-c.
Partager

| Plus
Du typhus d'Amérique ou fièvre jaune
Auteur(s) : Bally, François-Victor (1775-1866)
Année de publication :

Partager

| Plus
La politique coloniale de la France : le Ministère des colonies depuis Richelieu
Auteur(s) : Duchêne, Albert (1866-19..)
Auteurs secondaires : Nanotaux, Gabriel
Année de publication :

Partager

| Plus
Bulletin officiel de la Guyane française
Année de publication :

Partager

| Plus
Dictionaire francois-caraibe
Auteur(s) : Breton, Raymond (1609-1679)
Année de publication :

Partager

| Plus
Histoire d'Haïti (Ile de Saint-Domingue), depuis sa découverte jusqu'en 1824, époque des dernières négociations entre la France et le gouvernement haïtien
Auteur(s) : Malo, Charles (1790-1871)
Année de publication :

Partager

| Plus
Almanach royal, année bissextile M.DCC.LXXXVIII présenté à sa majesté pour la première fois en 1699
Auteur(s) : Houry, Laurent d' (1644-1725)
Auteurs secondaires : Debure, François-Jean-Noël (1743-1802)
Année de publication :

Partager

| Plus
Dictionnaire géographique et administratif universel d'Haïti illustré... ou Guide général en Haïti : avec gravures, illustrations, plans, cartes et vues dans le texte, et une carte coloriée de l'île d'Haïti. Tome 2, G à H
Auteur(s) : Rouzier, Sémexan
Année de publication :

Partager

| Plus
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
Bulletin officiel de la Guyane française
Année de publication :

Partager

| Plus
L'effort colonial français
Auteur(s) : Lebrun, Albert (18..-.... ; juriste)
Auteurs secondaires : Comité L'effort de la France et de ses alliés
Année de publication :

Partager

| Plus