FJ Millero, S Sotolongo, M Izaguirre - Geochimica et Cosmochimica Acta, 1987 - Elsevier
The oxidation of Fe (II) has been studied as a function of pH (5 to 9), temperature (5 to 45°
C), and salinity (0 to 35). The pseudo-first-order rate constant, k 1,− d [Fe (II)] dt= k 1 [Fe (II)] …