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Benthic manganese fluxes

Sundby, B., Silverberg, N., 1985. Manganese fluxes in the benthic boundary layer. Limnology and Oceanography, 30 372-381. [Pg.269]

McCaffrey, R.3., Myers, A.C., Davey, E., Morrison, G., Bender, M., Luedtke, N., Cullen, D., Froelich, P. and Klinkhammer, G., 1980. The relation between pore water chemistry and benthic fluxes of nutrients and manganese in Narragansett Bay, Rhode Island. Limnol. Oceanogr., 25(1) 31-44. [Pg.120]

Stirring within a flux-chamber controls the thickness of the benthic boundary layer and thus the diffusive flux of oxygen into the sediment. A decrease or even an intermption of stirring results in a significant increase of benthic efflux of redox-sensitive constituents such as iron and manganese. [Pg.253]

See other pages where Benthic manganese fluxes is mentioned: [Pg.262]    [Pg.408]    [Pg.891]    [Pg.3604]    [Pg.114]    [Pg.125]    [Pg.226]    [Pg.253]    [Pg.580]   
See also in sourсe #XX -- [ Pg.404 ]



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