The flux of soluble organic‐iron(III) complexes from sediments represents a source of stable iron(III) to estuarine waters and to the continental shelf

Publisher： John Wiley & Sons Inc

E-ISSN： 1939-5590|56|5|1811-1823

ISSN： 0024-3590

Source： LIMNOLOGY AND OCEANOGRAPHY, Vol.56, Iss.5, 2011-09, pp. : 1811-1823

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