A critical review of abiotic and microbially-mediated chemical reduction rates of Fe(III) (oxyhydr)oxides using a reactivity model

The reactivity of Fe (oxyhydr)oxides in reducing surface and sub-surface environments is a key factor controlling contaminant (e.g., As, U, Cr) solubility in natural waters and is also coupled tightly to multiple biogeochemical cycles (e.g., Fe, C, 5, and P). The reactivity model (J/m(0) = le(m/m(0))(gamma)) has been extensively applied to predict the reduction kinetics of synthetic minerals and natural sediments. This critical review has compiled abiotic (155 experiments) and biotic (162 experiments) Fe(III) reduction in the presence or absence of added organic matter to quantify the apparent reaction order (gamma value) and apparent reaction rate constant (k') of both natural and synthetic Fe(III) (oxyhydr)oxides. We found that both natural and synthesized Fe(III) (oxyhydr)oxides presented a range of gamma and k' values towards biotic Fe(III) reduction, indicating that the heterogeneity in Fe(III) (oxyhydr) oxides are critical in providing a proxy for abiotic Fe(III) reduction kinetics. While considerable errors may arise when the abiotic gamma and k' values of synthesized Fe(III) (oxyhydr)oxides are used to represent the gamma and k' values of natural Fe(III) (oxyhydr)oxides where microbes are present. Similar microbially mediated median gamma and k' values of natural and synthesized Fe(III) (oxyhydr)oxides highlight that microbial parameters significantly control the microbial Fe(III) reduction kinetics in addition to the heterogeneity in Fe(III) (oxyhydr)oxides (including the impurities and secondary Fe(III/II) mineralization, etc.), emphasizing the importance of microbial reactivities in better modelling the multiple biogeochemical cycle of Fe(III) (oxyhydr)oxides as well as the fate of contaminants solubility in global terrestrial and aquatic ecosystems.

Automated summary

The study revealed a range of gamma and k' values in both natural and synthesized Fe(III) (oxyhydr)oxides, crucial for providing a proxy for abiotic Fe(III) reduction kinetics. Microbial parameters significantly influence the microbial Fe(III) reduction kinetics in addition to the heterogeneity in Fe(III) (oxyhydr)oxides, emphasizing the importance of microbial reactivities in better modeling the biogeochemical cycles of Fe(III) (oxyhydr)oxides as well as the fate of contaminants solubility in global terrestrial and aquatic ecosystems.