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

Fig. 1.

Fig. 1

Comparison of the solubility of Fe(III) (mol L− 1) as a function of pH in synthetic seawater (present study, blue squares) and in 0.7 M NaCl (data points from Liu and Millero, 1999) at 25 °C. Data points of the present study represent the average of three measurements that agreed to ± 15%.