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The Aging Process of Cadmium in Paddy Soils under Intermittent Irrigation with Acid Water

A Short-Term Simulation Experiment

Bibliographic Data

ID15466004
AuthorsDongya Han (China Geological Survey), Lixin Pei (0000-0003-0069-0083, China Geological Survey, corresponding author), Guanxing Huang (0000-0003-0538-0690, China Geological Survey, corresponding author), Qinxuan Hou (Hebei GEO University), Meng Zhang (0000-0002-4822-2273, China Geological Survey), Jiangmin Song (China Geological Survey), Lin Gan (0000-0001-6107-663X, Chinese Academy of Geological Sciences), Heqiu Wu (Zhejiang Engineering Geophysical Survey and Design Institute Co., Ltd., Hangzhou 310005, China)
Year2022
Volume19
Issue6
Pages3339-3339
Publication date2022-03-11
Open AccessYes
TypeARTICLE
VenueInternational Journal of Environmental Research and Public Health (JOURNAL)
Journal identifiersISSN: 1661-7827 • E-ISSN: 1660-4601
PublisherMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/ijerph19063339
PMID35329022
OpenAlexW4220784550
LanguageEN
References cited51

Cadmium (Cd)-contaminated paddy soils are a big concern. However, the effect of irrigation with acid water on the migration and transformation of Cd and the effect of alternating redox conditions caused by intermittent irrigation on Cd aging processes in different depths of paddy soils are unclear. This study revealed Cd fractionation and aging in a Cd-contaminated paddy soil under four irrigation periods with acid water and four drainage periods, by applying a soil columns experiment and a sequential extraction procedure. The results showed that the dynamic changes of soil pH, oxidation reduction potential (ORP), iron (Fe) oxides and dissolved organic carbon (DOC) throughout the intermittent irrigation affected the transformation of Cd fractions. After 32 days, the proportion of exchangeable Cd (F1) to the total Cd decreased with a reduction of 24.4% and 20.1% at the topsoil and the subsoil, respectively. The labile fractions of Cd decreased, and the more immobilizable fractions of Cd increased in the different depths of soils due to the aging process. Additionally, the redistribution of the Fe and Mn oxide-bound Cd (F3) and organic matter and secondary-sulfide-bound Cd (F4) occurred at different depths of soils during the incubation time. Overall, the bioaccessibility of Cd in the subsoil was higher than that in the topsoil, which was likely due to the leaching and accumulation of soluble Cd in the deep soil. In addition, the aging processes in different depths of soils were divided into three stages, which can be mainly described as the transformation of F1 into F3 and F4

Agronomy · Cadmium · Fractionation · Irrigation · Leaching (pedology · Organic matter · Soil water · Subsoil · Topsoil · Chemistry · Chromium effects and bioremediation · Environmental Science · Heavy Metal Exposure and Toxicity · Heavy metals in environment · Environmental Chemistry · Soil Science

  • Sequential extraction procedure for the speciation of particulate trace metals

    Andre Tessier, Peter G C Campbell et al.•Analytical Chemistry•1979

Highly citedNo

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