Free Radicals Produced from the Oxidation of Ferrous Sulfides Promote the Remobilization of Cadmium in Paddy Soils During Drainage
| Autor: | Hui Huang, Peng Wang, Xiao-Bo Ji, Fang-Jie Zhao, Liang-Yi Cheng |
|---|---|
| Rok vydání: | 2021 |
| Předmět: |
Free Radicals
Radical chemistry.chemical_element 010501 environmental sciences Sulfides 01 natural sciences Ferrous Metal chemistry.chemical_compound Soil Environmental Chemistry Soil Pollutants Sulfate Dissolution 0105 earth and related environmental sciences Cadmium Oryza General Chemistry Sulfur chemistry Environmental chemistry visual_art Soil water visual_art.visual_art_medium Oxidation-Reduction |
| Zdroj: | Environmental sciencetechnology. 55(14) |
| ISSN: | 1520-5851 |
| Popis: | Most of the cadmium (Cd) accumulated in rice grains is derived from its remobilization in soils during the grain filling period when paddy water is drained. The factors affecting Cd remobilization upon drainage remain poorly understood. Here, we show that the free radical effect produced from the oxidation of ferrous sulfides is an important mechanism affecting the oxidative remobilization of Cd during soil drainage. When soils were flooded, microbial sulfate reduction results in the formation of various metal sulfides including CdS and FeS. Upon soil drainage, the oxidation of FeS produced considerable amounts of hydroxyl free radicals (OH•), which could oxidize CdS directly and thereby promote the oxidative dissolution of CdS and increase Cd mobilization in soils. FeS and CdS could also form a within-sulfide voltaic cell, with FeS protecting the oxidative dissolution of CdS due to the lower electrochemical potential of the former. However, this voltaic effect was short-lived and was surpassed by the free radical effect. The amounts and composition of metal sulfides formed during soil flooding vary with soils, and the oxidative dissolution of CdS is affected by both the free radical and voltaic effects offered by different metal sulfides. These effects are also applicable to the biogeochemistry of other chalcophile trace elements coupled with sulfur and iron redox cycles during the anoxic-oxic transition in many environments. |
| Databáze: | OpenAIRE |
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