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Keybot 13 Results  www.glf.dfo-mpo.gc.ca  Page 5
  ARCHIVà‰ - Lignes direc...  
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a) aux usines situées dans des secteurs où il est impossible de rejeter l'effluent sous la ligne de marée basse, par exemple, aux endroits ou le flux de la marée est important,
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(a) plant located in areas where discharge below low water mark is impractical, for example, in areas with a particularly high tidal reach,
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Les courants de marée sont attribuables au flux et au reflux de la mer. Le mascaret de réputation mondiale qu'on peut observer dans les cours d'eau à marée de la baie de Fundy est un excellent exemple de ce type de courant.
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Tidal currents result from the ebb and flow of the tide. An excellent example of this is the world renowned tidal bore that can be observed in the tidal rivers of the Bay of Fundy.
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Le flux et le reflux des eaux turbulentes sur les roches intertidales regorgent d'oxygène, de dioxyde de carbone, de substances nutritives dissoutes et de débris organiques, ce qui répond amplement à leurs besoins.
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Seaweed and sessile animals live in the intertidal zone because many of their predators can't live there. Turbulent water that ebbs and flows over the intertidal rocks is rich in oxygen, carbon dioxide, dissolved nutrients, and organic debris, providing abundantly for their needs.
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Toutefois, dans des endroits comme la baie de Fundy, où l'embouchure de la baie est large et profonde et où le fond de la baie est étroit et peu profond, lorsque les marées de mortes-eaux s'avancent, un fort volume d'eau est refoulé dans un goulet plus étroit. Par conséquent, même durant les marées de mortes-eaux, le flux monte plus haut sur les côtes et le reflux tombe plus bas que n'importe où ailleurs dans la région de l'Atlantique.
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However, in places like the Bay of Fundy, where the mouth of the bay is wide and deep and the head of the bay is narrow and shallow, when the neap tide advances, a large volume of water has to fit into a smaller space. As a result, even during neap tides the water rises higher and falls lower along the Fundy shore than other places in Atlantic Canada.
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Le long d'un rivage rocailleux, le flux et le reflux de la marée peuvent se situer n'importe où entre 3 et 12 mètres. Cette amplitude de l'action des marées crée des zones. Toutes les zones sont différentes les unes des autres selon la température, la salinité, l'exposition au vent et à la lumière et la période de temps durant laquelle la zone est recouverte par la mer.
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Along a rocky shoreline the rise and fall of the tide may be anywhere from 3-12 metres. This magnitude of tidal action creates zones. Each zone is different from the next, depending on the temperature, salinity, exposure to wind and light, and the amount of time the zone is covered by the sea. The living beings that occupy these zones are especially adapted to their living conditions. They have special ways of staying put and preventing themselves from drying out at low tide.
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Compte tenu de ces forces antagonistes, il est difficile de prévoir si l'amplitude de la marée sera moindre ou supérieure à la tête de l'estuaire. Le flux et le reflux des marées peuvent se ressentir très loin en amont, en particulier dans les grands estuaires.
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The American Oyster requires a temperature of 20° C, while the Bay Quahaug requires 23° C to breed. It is not surprising that the distribution boundary for the Bay Quahaug is more to the south than the one for the American Oyster. In fact, oysters are found as far north as Caraquet Bay, New Brunswick, while the Bay Quahaug is only found as far north as the Miramichi estuary, New Brunswick.
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Les eaux sont également turbulentes à proximité de la terre ferme, entre diverses petites îles dont celles de Campobello et de Deer. Des chenaux assez étroits et l'emplacement aléatoire des îles créent un véritable labyrinthe pour le flux et le reflux des eaux de marée.
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The East Coast of Canada is influenced greatly by water masses, mainly the cold Labrador current flowing out of the Arctic, the St. Lawrence River flowing into its Gulf, and the tides of the Bay of Fundy. The warm northeasterly flowing Gulf Stream current flows hundreds of kilometres offshore. It often influences the waters of Georges Bank, Brown's Bank, and parts of the Scotian Shelf through eddies or 'warm core rings.' It mixes with the cold Labrador current over the Grand Banks and creates large upwellings.
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Ceci est en accord avec Fabiano et al. (2003) qui ont découvert que la réaction bactérienne et la dégradation des MO durant la bioremédiation des sédiments étaient plus évidentes dans l’eau sus-jacente due au flux benthique-pélagique du carbone dissous mobilisé dans les sédiments.
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Although the sediment of the ORC box showed an increase in βG, CSEA, Eh, and pH (Figs. 1–3), the lack of evidence for a OM decrease (Fig. 3) may be explained by the excessive sedimentary organic load. An additional reason for the lack of CHO degradation could be due to the microcosms’ operating conditions: OM, once mobilized, is not removed (because of the closed system) and may sink back to the sediment. However, the overall functional and structural response observed using ORC compounds (both in the water and in the sediment compartments) supports the evidence for an increased OM degradation in the sediment compartment. In particular, the significant effect recorded in the water compartment suggests the occurrence of a strong benthic–pelagic coupling (ORC socks were positioned within the sediment). This implies a mobilization of OM in the sediment that, once released into the water column, may stimulate a prompt response by the bacterial community. This is in accord with Fabiano et al. (2003) who found that bacterial response and OM degradation during bioremediation of sediment was more evident in the overlying water due to the benthic–pelagic flux of dissolved carbon mobilized in the sediment.