Iron
(hydr)oxides are the most abundant metal oxides, which are
widespread on Earth’s surface in the major form of micro/nanoparticles.
Dissolution of iron (hydr)oxides significantly controls their compositions
on Earth’s surface and is a critical step for the global Fe
cycling. Photoreductive dissolution of iron (hydr)oxides is recognized
as one of the most important process for generating Fe2+ in surface water and is also a common pathway for transforming solar
energy into chemical energy. This review article dissects the main
characteristics of photoreductive dissolution of iron (hydr)oxides
and discusses its geochemical and environmental significance. We categorize
the mechanisms for photoreduction of iron (hydr)oxides into three
types: reduction by intrinsic photogenerated electrons, reduction
by ligand to metal electron transfer (LMCT), and reduction by direct
injection of exogenous photoelectrons. The efficiency of photoreductive
dissolution is constrained by both the structure of iron (hydr)oxides
(e.g., crystal structure and particle size) and environmental conditions
(e.g., light, pH, and concurrent chemicals). Therefore, different
iron (hydr)oxides may exhibit quite distinctive photoreductive dissolution
characteristics because of their unique crystal structures and physicochemical
properties. Iron (hydr)oxides with low crystallinity (e.g., ferrihydrite,
lepidocrocite) are subject to direct photoreductive dissolution, while
those with high crystallinity (e.g., goethite, hematite) generally
need ligands to proceed with photoreductive dissolution. The photoreductive
dissolution of iron (hydr)oxides is involved in many important geochemical
and environmental processes, such as the Fe availability to primary
producers, the generation of reactive oxygen species, the transportation
and fate of contaminants, and the phase transformation of iron (hydr)oxides.
Given the ubiquitous occurrence of photoreductive dissolution of iron
(hydr)oxides, this review will advance our understanding of the role
of this process in Earth’s surface environments.