Photoexcitation
of natural semiconductor Fe(III) minerals has been
proven to generate Fe(II), but the photogeneration of Fe(II) in Fe-rich
surface soil as well as its role in the redox biogeochemistry of Cr(VI)
remains poorly understood. In this work, we confirmed the generation
of Fe(II) in soil by solar irradiation and proposed a new mechanism
for the natural reductive detoxification of Cr(VI) to Cr(III) in surface
soil. The kinetic results showed that solar irradiation promoted the
reduction of Cr(VI) in Fe-rich soils, while a negligible Cr(VI) reduction
was observed in the dark. Fe(II), mainly in the form of silicate-bound
Fe(II), was generated under solar irradiation and responsible for
the reduction of Cr(VI) in soils, which was evidenced by sequential
extraction, transmission electron microscopy with electron energy
loss spectroscopy, and electron transfer calculation. Photogenerated
silicate-bound Fe(II) resulted from the massive clay–iron (hydr)oxide
associations, consisting of iron (hydr)oxides (e.g., hematite and
goethite) and kaolinite. These associations could generate Fe(II)
under solar irradiation either via intrinsic excitation to produce
photoelectrons or via the ligand-to-metal charge transfer process
after the formation of clay–iron (hydr)oxide–organic
matter complexes, which was proven by photoluminescence spectroscopy
and X-ray photoelectron spectroscopy. These findings highlight the
important role of photogenerated Fe(II) in Cr(VI) reduction in surface
soil, which advances a fundamental understanding of the natural detoxification
of Cr(VI) as well as the redox biogeochemistry of Cr(VI) in soil.