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  2. Benthic-pelagic coupling - Wikipedia

    en.wikipedia.org/wiki/Benthic-pelagic_coupling

    Benthic-pelagic coupling are processes that connect the benthic zone and the pelagic zone through the exchange of energy, mass, or nutrients. These processes play a prominent role in both freshwater and marine ecosystems and are influenced by a number of chemical, biological, and physical forces that are crucial to functions from nutrient cycling to energy transfer in food webs.

  3. Sediment–water interface - Wikipedia

    en.wikipedia.org/wiki/Sediment–water_interface

    The availability of a variety of lake contaminants is determined by which reactions are taking place within the freshwater system. Chemical reactions at the sediment water interface are listed here below: Oxygen consumption- O 2--> H 2 O; Denitrification- NO 3--> N 2; Manganese reduction- Mn IV--> Mn II; Iron reduction- Fe III--> Fe II; Sulfate ...

  4. Benthic zone - Wikipedia

    en.wikipedia.org/wiki/Benthic_zone

    As with oceans, the benthic zone is the floor of the lake, composed of accumulated sunken organic matter. The littoral zone is the zone bordering the shore; light penetrates easily and aquatic plants thrive. The pelagic zone represents the broad mass of water, down as far as the depth to which no light penetrates. [9]

  5. Benthic boundary layer - Wikipedia

    en.wikipedia.org/wiki/Benthic_boundary_layer

    The benthic boundary layer (BBL) plays a vital role in the cycling of matter and is commonly referred to as the “endpoint” or "sink" for sediment material, which fuels high metabolic rates for microbial populations. [7] The particles from the pelagic ecosystem sink to the BBL where they will be used by organisms. [2]

  6. Pelagic zone - Wikipedia

    en.wikipedia.org/wiki/Pelagic_zone

    Altogether, the pelagic zone occupies 1,330 million km 3 (320 million mi 3) with a mean depth of 3.68 km (2.29 mi) and maximum depth of 11 km (6.8 mi). [2] [3] [4] Pelagic life decreases as depth increases. The pelagic zone contrasts with the benthic and demersal zones at the bottom of the sea. The benthic zone is the ecological region at the ...

  7. Neighbouring group participation - Wikipedia

    en.wikipedia.org/wiki/Neighbouring_group...

    In this type of substitution reaction, one group of the substrate participates initially in the reaction and thereby affects the reaction. A classic example of NGP is the reaction of a sulfur or nitrogen mustard with a nucleophile, the rate of reaction is much higher for the sulfur mustard and a nucleophile than it would be for a primary or secondary alkyl chloride without a heteroatom.

  8. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Water is the medium of the oceans, the medium which carries all the substances and elements involved in the marine biogeochemical cycles. Water as found in nature almost always includes dissolved substances, so water has been described as the "universal solvent" for its ability to dissolve so many substances.

  9. Midwater trawling - Wikipedia

    en.wikipedia.org/wiki/Midwater_trawling

    Midwater (pelagic) otter trawl 1: trawl warp, 2: otter boards, 3: longline chains, 4 hunter, 5: weights 6: headline with floats, 7: pre-net, 8: tunnel and belly, 9: codend Midwater trawling is trawling , or net fishing, at a depth that is higher in the water column than the bottom of the ocean.