氧化还原
镉
生物利用度
溶解
土壤水分
环境化学
水田
环境科学
化学
农学
土壤科学
无机化学
生物
有机化学
生物信息学
物理化学
作者
Chunhua Zhang,Ying Ge,Huan Yao,Xiao Chen,Minkun Hu
标识
DOI:10.1007/s11783-012-0394-y
摘要
Redox conditions in paddy soils may vary as they are submerged and drained during rice growth. This change may bring about reductive dissolution of iron (Fe) oxides and subsequent formation of secondary Fe-bearing minerals in rice paddies. The mobility and bioavailability of metal contaminants such as cadmium (Cd) in paddy soils are closely related to the chemical behaviors of Fe. Therefore, in this paper, advances in the study of paddy Fe redox transformations and their effects on Cd availability to rice are briefly reviewed. Current concepts presented in this review include the forms of Fe in paddy soils, the reactions involved in Fe oxidation-reduction, chemical factors affecting Fe redox processes, Cd availability to rice and the impacts of Fe transformation on Cd uptake and translocation in rice. Prospects for future research in this area are also discussed.
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