Jiali Yan, Xuwei Li, Jintao Li, Jiankang Zhou, Jiamin Shi, Kangfu Liu, Xin Chen, Shiqi Zhou, Weiwei Sun, Fuqing Sui, Xiaochen Lin, Lei Zhang, Matthew H. H. Fischel
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引用次数: 0
Abstract
Background and aims
Red mud, an alkaline byproduct of aluminum smelting, can serve as a soil amendment to mitigate soil cadmium contamination. Rice uptakes cadmium mainly during the grain-filling stage after soils are drained. During the flooding-drainage process, substantial fluctuations in redox potential occur, and the effectiveness of red mud amendment under these conditions remains unresolved. The aim is to test the effects of red mud on soil cadmium mobility after soil drainage and subsequent rice cadmium accumulation.
Methods
Soil cadmium fractions and release kinetics were assessed by sequential extraction and stirred-flow experiments followed by soil microcosm incubation with slightly cadmium-contaminated paddy soil (0.52 mg Cd kg−1), respectively. Rice cadmium accumulation was assessed in a potted rice experiment.
Results
Incorporating up to 2% red mud enhanced the proportions of cadmium bound to iron and manganese oxides from 12.5–28.1% to 25.1–44.0%, thus effectively reducing the mobility of cadmium in paddy soil after soil drainage. As a result, cadmium contents were decreased by 72.5–76.9% and 84.7–91.2% in the rice grains and straw, respectively.
Conclusions
Applying 2% red mud enhanced the soil iron and manganese oxide-cadmium proportions after soil drainage, decreasing the soil cadmium release maximum and rate, limiting cadmium uptake and subsequent accumulation into the rice grain to a level permissible for human ingestion. The stability of iron minerals impacts soil cadmium adsorption. These findings provide a scientific basis for using red mud in paddy soil cadmium remediation.
期刊介绍:
Plant and Soil publishes original papers and review articles exploring the interface of plant biology and soil sciences, and that enhance our mechanistic understanding of plant-soil interactions. We focus on the interface of plant biology and soil sciences, and seek those manuscripts with a strong mechanistic component which develop and test hypotheses aimed at understanding underlying mechanisms of plant-soil interactions. Manuscripts can include both fundamental and applied aspects of mineral nutrition, plant water relations, symbiotic and pathogenic plant-microbe interactions, root anatomy and morphology, soil biology, ecology, agrochemistry and agrophysics, as long as they are hypothesis-driven and enhance our mechanistic understanding. Articles including a major molecular or modelling component also fall within the scope of the journal. All contributions appear in the English language, with consistent spelling, using either American or British English.