Literatura científica selecionada sobre o tema "Sédiments marins – Teneur en composés organiques – Martinique (France)"
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Teses / dissertações sobre o assunto "Sédiments marins – Teneur en composés organiques – Martinique (France)":
Jalaluddin, Noor. "Origine, nature et distribution des hydrocarbures dans des sendiments marins tropicaux (Martinique et Guadeloupe) et équatoriaux (Indonésie)". Aix-Marseille 3, 1992. http://www.theses.fr/1992AIX30042.
Lerat, Yannick. "Cycles annuels de la matière organique et des éléments nutritfs dans les sédiments d'un écosystème côtier (baie de Morlaix, France) : interactions avec le compartiment pélagique". Brest, 1990. http://www.theses.fr/1990BRES2004.
Gomez, Hernandez Maria Elena. "Rôle des sédiments dans l'eutrophisation d'une lagune littorale Méditerranéenne (étang du Méjean-Hérault) : échanges du phosphate entre le sédiment et l'eau en fonction des conditions environnementales". Montpellier 1, 1996. http://www.theses.fr/1996MON13520.
Mesnage, Valérie. "Contribution à l'étude de la mobilité des formes de phosphate à l'interface eau-sédiment dans les écosystèmes lagunaires". Montpellier 1, 1994. http://www.theses.fr/1994MON13508.
Chaumery, Christian. "Répartition des éléments nutritifs sur le plateau continental armoricain et en mer d'Iroise en relation avec le régime hydrique de la Loire : Assimilation Régénération. Facteurs limitant la production phytoplanctonique". Brest, 2004. http://www.theses.fr/2004BRES2020.
The spreading of low-saline nutrient-rich waters of the Loire estuary as tidally-regulated meanders injects nutrients over a major part of the Armorican continental shelf region in winter. The nutrients thus brought in are consumed in spring as the river plume spreads over the shelf. The magnitude of the flux of nutrients transported by the Loire in the south Brittany sector varies according to the intensity of river discharge and the timing of the peak discharge(s). Addition of nutrients with high flows in spring alleviates nutrient limitation and enhances primary production. When the spring river discharge is strong and occurs over a long period, the Loire waters could be distinctly differentiated from surrounding Iroise Sea waters. The Loire waters circumnavigate the Ouessant Island by the west and penetrate into the western English Channel. A study of the distribution nutrients on the Armorican continental shelf also enables identification of various sectors subjected to nutrient addition with freshwaters: Loire, Gironde, and Vilaine. Using nutrients as tracers of the circulation of the Loire waters on the Armorican continental shelf, the average velocity of displacement of the Loire plume from its estuary to Ouessant island has been estimate at 5 cm. S-1. Assimilation of nitrogen and phosphorus by the phytoplankton occurs in a ratio close to that of the Redfield ratio (N/P=16). Ratios of assimilation of nitrogen and silicon decrease with time indicating the increasing importance of regenerated production. In the cold deep water of the South Brittany, regeneration of nutrients begins in the southeastern part. Regeneration of silicon begfins as early as April and is twice faster than that of nitrate