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Depletable peroxidase-like activity of Fe3O4 nanozymes accompanied with separate migration of electrons and iron ions.


ABSTRACT: As pioneering Fe3O4 nanozymes, their explicit peroxidase (POD)-like catalytic mechanism remains elusive. Although many studies have proposed surface Fe2+-induced Fenton-like reactions accounting for their POD-like activity, few have focused on the internal atomic changes and their contribution to the catalytic reaction. Here we report that Fe2+ within Fe3O4 can transfer electrons to the surface via the Fe2+-O-Fe3+ chain, regenerating the surface Fe2+ and enabling a sustained POD-like catalytic reaction. This process usually occurs with the outward migration of excess oxidized Fe3+ from the lattice, which is a rate-limiting step. After prolonged catalysis, Fe3O4 nanozymes suffer the phase transformation to γ-Fe2O3 with depletable POD-like activity. This self-depleting characteristic of nanozymes with internal atoms involved in electron transfer and ion migration is well validated on lithium iron phosphate nanoparticles. We reveal a neglected issue concerning the necessity of considering both surface and internal atoms when designing, modulating, and applying nanozymes.

SUBMITTER: Dong H 

PROVIDER: S-EPMC9467987 | biostudies-literature | 2022 Sep

REPOSITORIES: biostudies-literature

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Depletable peroxidase-like activity of Fe<sub>3</sub>O<sub>4</sub> nanozymes accompanied with separate migration of electrons and iron ions.

Dong Haijiao H   Du Wei W   Dong Jian J   Che Renchao R   Kong Fei F   Cheng Wenlong W   Ma Ming M   Gu Ning N   Zhang Yu Y  

Nature communications 20220912 1


As pioneering Fe<sub>3</sub>O<sub>4</sub> nanozymes, their explicit peroxidase (POD)-like catalytic mechanism remains elusive. Although many studies have proposed surface Fe<sup>2+</sup>-induced Fenton-like reactions accounting for their POD-like activity, few have focused on the internal atomic changes and their contribution to the catalytic reaction. Here we report that Fe<sup>2+</sup> within Fe<sub>3</sub>O<sub>4</sub> can transfer electrons to the surface via the Fe<sup>2+</sup>-O-Fe<sup>3+<  ...[more]

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