The
homogeneous Fe-catalyzed Fenton reaction remains an attractive
advanced oxidation process for wastewater treatment, but sustaining
the Fe(III)/Fe(II) redox cycle at a convenient pH without the costly
input of energy or reductants remains a challenge. Mn(II) is known
to accelerate the Fenton reaction, yet the mechanism has never been
confidently established. We report a systematic kinetic and spectroscopic
investigation into Mn(II) acceleration of atrazine or 2,4,6-trichlorophenol
degradation by the picolinic acid (PICA)-assisted Fenton reaction
at pH 4.5–6.0. Mn(II) accelerates Fe(III) reduction, superoxide
radical (HO2
•/O2
•–) formation, and hydroxyl radical (HO•) formation.
A Mn(II/III)-H2O2 redox cycle as an independent
source of reactive oxygen species, as proposed in the literature,
is shown to be insignificant. Rather, Mn(II) assists by participating
directly and catalytically in the Fe(III)/Fe(II) redox cycle. Initially,
Mn(II) (as MnII(PICA)+) complexes with a ferric
hydroperoxo species, PICA-FeIII-OOH. The resulting binuclear
complex undergoes intramolecular electron transfer to give Fe(II),
which later generates HO• from H2O2, plus MnO2
+, which later decomposes
to HO2
•/O2
•– (an Fe(III) reductant) and Mn(II), completing the catalytic cycle.
This scheme may apply to other Fenton-type systems that go through
an FeIII-OOH intermediate. The findings here will inform
the design of practical and sustainable Fenton-based AOPs employing
Mn(II) in combination with chelating agents.