Isotope exchange between iron(II or III) hydroxide and HTO water in the equilibrium state

Observing the OT-for-OH exchange reaction between iron(II or III) hydroxide and tritiated water (HTO) leads to the following results: (1) isotope exchange as atomic group occurred between the OH group in each iron hydroxide (i.e., Fe(OH)₂ or Fe(OH)₃) and OT^– resulted from the dissociation of HTO; (2) the ratio of the reactivity of the hydroxides is roughly iron(III) hydroxide]: iron(II) hydroxide]=1.21.0 and the result is related to a difference in electronegativity between Fe²⁺ and Fe³⁺. (In other words, if the reactivity depends on the number of the charge, the ratio should be 1.51.0).