Uic model 5011 coulometer manual

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Transport-reaction modeling of dissolved metabolite concentrations will allow us to quantify rates of principal net activities in the sediment (e.g., reductions of O, Mn[IV], and Fe[III]) (Jørgensen, 2006).

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Concentration data will also allow us to calculate mineral stabilities and, in anoxic sediment, to test thermodynamic models of metabolic competition (Hoeer et al., 2000; Wang et al., 2010).

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Chemical data (e.g., the position of the coride maximum from the Last Glacial Maximum) and thermal data will be used to help model this transport (D’Hondt et al., 2004).

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We undertook key biogeochemical analyses on the ship and collected appropriate samples for critical postcruise biogeochemical studies.


Uic model 5011 coulometer manual:

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