Using224Ra/228Th disequilibrium to examine transport processes controlling the benthic fluxes of DIC

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Depth profiles of dissolved and surface-bounded 224Ra as well as 228Th in near-surface sediment were determined at several sites in the Pearl River estuary (PRE) and the adjacent South China Sea (SCS) shelf.Together with 224Ra and 228Th measurements,dissolved inorganic carbon (DIC) and dissolved inorganic nitrogen (NO3+NO2,NH4+) in porewater and the overlying water were also measured.
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