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. 2015 Aug 20;174:85–93. doi: 10.1016/j.marchem.2015.05.009

Table 3.

Conditional complex stability constants for Fe(III) complexes with seawater-soluble riverine NOM in seawater.

NOM fraction Method NOM concentration during measurements (mg L− 1) Log Kcond Reference
Suwannee River fulvic acid Competing ligand/UV–Vis 10 10.4 Rose and Waite (2003)
Suwannee River fulvic acid Competing ligand/cathodic stripping voltammetry 1–4 10.6 ± 0.2 Laglera and van den Berg (2009)
Suwannee River NOM fraction SR_0 Radiotracer technique 0.0005–0.004 10.6 ± 0.4 Present work
Suwannee River NOM fraction SR_1 Radiotracer technique 0.0005–0.004 9.7 ± 0.6 Present work
Suwannee River NOM fraction SR_2 Radiotracer technique 0.0005–0.004 9.5 ± 0.6 Present work
Peat-bog draining creek NOM fraction TM_0 Radiotracer technique 0.0005–0.004 10.4 ± 0.4 Present work
Peat-bog draining creek NOM fraction TM_1 Radiotracer technique 0.0005–0.004 10.5 ± 0.6 Present work
Peat-bog draining creek NOM fraction TM_2 Radiotracer technique 0.0005–0.004 9.5 ± 0.6 Present work
Peat-bog draining creek NOM fraction CB_0 Radiotracer technique 0.0005–0.004 9.8 ± 0.6 Present work
Peat-bog draining creek NOM fraction CB_1 Radiotracer technique 0.0005–0.004 8.8 ± 0.6 Present work
Peat-bog draining creek NOM fraction CB_2 Radiotracer technique 0.0005–0.004 8.5 ± 0.6 Present work