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36 μmol g-1 of DIP was adsorbed to clay minerals. In November (non-hypoxia season), however, ~0.54 μmol g-1 of OP was converted into DIP, while ~0.55 μmol g-1 and ~0.28 μmol g-1 of DIP was adsorbed to clay minerals and bind to iron oxides. Furthermore, scallop farming activities also affected the P mobilization through biological deposition and reduced hydrodynamic conditions. The burial fluxes of P varied from 11.67 to 20.78 μmol cm-2 yr-1 and its burial efficiency was 84.7-100%, which was consistent with that in most of the marginal s
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