Abstract
The coupling relationship between the <1 kDa, 1–3 kDa, 3–10 kDa, 10–100 kDa, and 100 kDa–0.45 μm Fe fractions and the environmental factors in the Bohai Sea (BS) was investigated. The 1–100 kDa Fe in the surface water exhibited a non-conservative phenomenon during the river–sea mixing process, which was related to the removal of colloidal Fe via flocculation during this process. For the bottom water, the ligands released by the sediments may form additions to the <100 kDa Fe. The COC and DOC were mainly closely related to the behavior of the Fe in the bottom water. The <1 and 3–10 kDa Fe was mainly significantly positively correlated with the DOC, while the <100 kDa–0.45 μm Fe was significantly negatively correlated with the DOC. <100 kDa LMW colloidal Fe exhibited more synergistic behavior with easily absorbed ammonium salts.
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