“…As illustrated, both free ( k fre ) and solid ( k sol ) Fe(II) react with O 2 to produce iron (oxyhydr)oxides and •OH, with free Fe(II) reacting at a higher rate than solid Fe(II), and solid Fe(II) in biogenic RIM reacting at a higher rate than in abiotic RIM. Higher rates of reaction with O 2 for free versus solid Fe(II) may be due to faster mass transfer of the former which is a homogeneous reaction, , and thermodynamic changes via the complexation of free Fe(II) with inorganic ions (i.e., carbonate), , organic ligands (from biomass), , and mineral surface association. , It should be noted that the mechanism for •OH production with free or solid Fe(II) in two-phase (i.e., liquid and solid) systems is well documented and yields O 2 •– , H 2 O 2 , and finally •OH. ,, …”