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The transport of excess atmospheric CO 2 (defined as the fraction of dissolved inorganic carbon (DIC) that can escape as CO 2 to the atmosphere due to water-air equilibration), by the five rivers entering the Scheldt estuary is investigated. Excess CO 2 originates from both respiration in the soil and the river and represents 10<space>% of the DIC and 6<space>%...
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