|
|
|
Registros recuperados: 10 | |
|
|
Martin, Jean-louis; Sornin, Jean-marc; Delmas, Daniel; El Sayed, Mohamed A.; Berthet, Brigitte. |
Au cours de cette étude, nous avons étudié l'impact de la biodéposition sur les bassins conchylicoles. La biodéposition constitue un "concentrateur" de particules fines au niveau du sédiment. Cet impact est particulièrement évident sur les sédiments sableux et concerne la granulométrie, les taux de matière organique, la concentration des métaux et des hydrocarbures. Une étude comparée est faite entre estran sableux et bassin de type "claire" à sédiment argileux. L'impact de la biodéposition sur les sédiments sableux n'est pas irréversible. Le bassin fermé avec un sédiment argileux agit comme un concentrateur-rétenteur de particules et des contaminants potentiels. Ceci souligne le rôle "tampon" des marais maritimes entre milieu continental et milieu marin. |
Tipo: Text |
|
Ano: 1989 |
URL: http://archimer.ifremer.fr/doc/00076/18757/16327.pdf |
| |
|
| |
|
|
Feuillet-girard, Michelle; Heral, Maurice; Sornin, Jean-marc; Deslous-paoli, Jean-marc; Robert, Jean-michel; Mornet, Francoise; Razet, Daniel. |
The respective influences of the sediment and of oyster (Crassostrea gigas) farming on the accumulation and the recycling of different forms of organic and inorganic nitrogen are described. Fluxes of dissolved inorganic and organic forms of nitrogen were studied between the water column, the water overlying the sediment and the pore waters, while for particulate forms the fluxes were studied between suspended material, the "biodeposits" (faeces and pseudofaeces of Crassostrea) and the sediment. The flux of inorganic nitrogen amounts to 10.5 106 g.m(-2). Yr(-1), while that of organic nitrogen is half this figure. The particulate flux is 15.106 g.m(-2).yr(-1). On the other hand, the phytoplanktonic nitrogen accounts for only 6% of the total particulate... |
Tipo: Text |
Palavras-chave: Marenne Oleron; Sediment; Pore water; Interface; Crassostrea gigas; Nitrogen; Marennes Oléron; Sédiment; Eau interstitielle; Adsorption; Interface; Crassostrea gigas; Azote. |
Ano: 1988 |
URL: http://archimer.ifremer.fr/doc/1988/publication-2878.pdf |
| |
|
|
Sornin, Jean-marc; Collos, Yves; Delmas, Daniel; Feuillet-girard, Michèle; Gouleau, Daniel. |
The oyster pond under study has a natural sediment bottom and water is changed only once or twice every month depending on tidal height. Between successive water renewals, the pond is a closed system, equivalent to a batch culture in which sinking and biodeposition of particulate matter are the only sources of organic matter to the bottom. Particulate organic matter enrichment of the sediment in winter is followed by intensive ammonification in summer with very limited nitrification. Seasonal nitrogen budgets involving particulate and dissolved phases show that in summer during batch mode period, ammonium enrichment from the sediment to the overlying water is an order of magnitude higher than the initial nutrient supply in the feed water. This allows a... |
Tipo: Text |
|
Ano: 1990 |
URL: http://archimer.ifremer.fr/doc/00178/28892/27749.pdf |
| |
|
| |
|
| |
|
|
Sornin, Jean-marc. |
Most shellfish farms are located in sheltered areas which enable farmers to work whatever the weather is like as well as to limit the damages caused by storms. But these areas get some important natural sediment deposits. Looking at the height of some muddy elevations which can ruin traditional on-bottom oyster farms, overelevation techniques have spread rapidly. Showing numerous advantages (easier handling, reduced carrying out by the sea, better oyster growth...), off-bottom culture is more and more used and tends to substitute completely on-bottom culture. However, this technique poses some important silting problems. Indeed, if these elevated cultures enable farmers to avoid mud deposits in the short-term, they quickly lead to a new sediment increase.... |
Tipo: Text |
|
Ano: 1982 |
URL: http://archimer.ifremer.fr/doc/1982/publication-6659.pdf |
| |
|
| |
Registros recuperados: 10 | |
|
|
|