High-valent iron-oxo species (Fe
IV
=O) has been a long-sought-after oxygen transfer reagent in biological and catalytic chemistry but suffers from a giant challenge in its gentle and selective synthesis. Herein, we propose a new strategy to synthesize surface Fe
IV
=O (≡Fe
IV
=O) on nanoscale zero-valent iron (nZVI) using chlorite (ClO
2
–
) as the oxidant, which possesses an impressive ≡Fe
IV
=O selectivity of 99%. ≡Fe
IV
=O can be energetically formed from the ferrous (Fe
II
) sites on nZVI through heterolytic Cl–O bond dissociation of ClO
2
–
via a synergistic effect between electron-donating surface ≡Fe
II
and proximal electron-withdrawing H
2
O, where H
2
O serves as a hydrogen-bond donor to the terminal O atom of the adsorbed ClO
2
–
thereby prompting the polarization and cleavage of Cl-O bond for the oxidation of ≡Fe
II
toward the final formation of ≡Fe
IV
=O. With methyl phenyl sulfoxide (PMS
16
O) as the probe molecule, the isotopic labeling experiment manifests an exclusive
18
O transfer from Cl
18
O
2
–
to PMS
16
O
18
O mediated by ≡Fe
IV
=
18
O. We then showcase the versatility of ≡Fe
IV
=O as the oxygen transfer reagent in activating the C-H bond of methane for methanol production and facilitating selective triphenylphosphine oxide synthesis with triphenylphosphine. We believe that this new ≡Fe
IV
=O synthesis strategy possesses great potential to drive oxygen transfer for efficient high-value-added chemical synthesis.