4.7 Article

Biogeochemical cycling in paddy soils controls antimony transformation: Roles of iron (oxyhydr)oxides, organic matter and sulfate

Journal

JOURNAL OF HAZARDOUS MATERIALS
Volume 464, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.jhazmat.2023.132979

Keywords

Antimony; Paddy soil; Iron (oxyhydr)oxides; Biogeochemistry; Kinetics

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This study investigates the transformation of antimony (Sb) in paddy fields and identifies the key processes involved. The results show that under anaerobic conditions, the release of Sb is facilitated by the reductive dissolution of iron, the release of soil colloids, and dissolved organic carbon. In the subsequent aerobic phase, the oxidation of Sb(III) by reactive oxygen species leads to increased levels of dissolved Sb(V). These findings contribute to a better understanding of the biogeochemical cycling of Sb in paddy systems.
In paddy fields, periodic flooding and drainage phases can significantly affect the availability of antimony (Sb), but the underlying mechanisms remain unclear. In this study, Sb-contaminated paddy soil was incubated under anaerobic (40 day) and subsequently aerobic (40-55 day) conditions. The Sb fractions was investigated and a kinetic model was established to quantitatively evaluate the main processes controlling Sb transformation. Under anaerobic conditions, the reductive dissolution of iron (Fe) (oxyhydr)oxides, the release of soil colloids, and dissolved organic carbon (DOC) could facilitate the release of Sb(V), while newly released Sb(V) were synchronously reduced to Sb(III) that could be incorporated into the solid phase (34.1%, 40 day) or precipitated as Sb2S3 (9.7%, 40 day). After soil aeration, a significant increase in dissolved and extracted Sb(V) (34.7%, 45 day) was observed due to the Sb(III) oxidization by the reactive oxygen species (ROS) generated from Fe(II) oxidization. The dissolved and extracted Sb(V) were simultaneously incorporated into the solid phase as the reaggregation of soil colloids and DOC, and only contributed to 17.1% of the total Sb content at the end of aerobic phase (55 day). Our results elucidated the mechanisms about how biogeochemical Fe/S/C cycling jointly controlled Sb transformation in paddy systems.

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