Enhanced sequestration of uranium by coexisted lead and organic matter during ferrihydrite transformation

被引:1
作者
Huang X. [1 ,2 ]
Ding Y. [1 ,3 ]
Zhu N. [2 ]
Li L. [1 ]
Fang Q. [1 ]
机构
[1] School of Resource & Environment and Safety Engineering, University of South China, Hunan, Hengyang
[2] School of Environment and Energy, Guangdong Provincial Key Laboratory of Solid Wastes Pollution Control and Recycling, South China University of Technology, Guangdong, Guangzhou
[3] Key Discipline Laboratory for National Defense for Biotechnology in Uranium Mining and Hydrometallurgy, University of South China, Hengyang
基金
中国国家自然科学基金;
关键词
Dissolved organic matter; Fe (oxyhydr)oxides; Fh transformation; Pb; U sequestration;
D O I
10.1016/j.chemosphere.2023.140041
中图分类号
学科分类号
摘要
The dynamic reactions of uranium (U) with iron (Fe) minerals change its behaviors in soil environment, however, how the coexisted constituents in soil affect U sequestration and release on Fe minerals during the transformation remains unclear. Herein, coupled effects of lead (Pb) and dissolved organic matter (DOM) on U speciation and release kinetics during the catalytic transformations of ferrihydrite (Fh) by Fe(II) were investigated. Our results revealed that the coexistence of Pb and DOM significantly reduced U release and increased the immobilization of U during Fh transformation, which were attributed to the enhanced inhibition of Fh transformation, the declined release of DOM and the increased U(VI) reduction. Specifically, the presence of Pb increased the coprecipitation of condensed aromatics, polyphenols and phenols, and these molecules were preferentially maintained by Fe (oxyhydr)oxides. The sequestrated polyphenols and phenols could further facilitate U(VI) reduction to U(IV). Additionally, a higher Pb content in coprecipitates caused a slower U release, especially when DOM was present. Compared with Pb, the concentrations of the released U were significantly lower during the transformation. Our results contribute to predicting U sequestration and remediating U-contaminated soils. © 2023 Elsevier Ltd
引用
收藏
相关论文
共 52 条
  • [1] Aeschbacher M., Graf C., Schwarzenbach R.P., Sander M., Antioxidant properties of humic substances, Environ. Sci. Technol., 46, pp. 4916-4925, (2012)
  • [2] Bao Y.P., Lai J.H., Wang Y.S., Fang Z., Su Y.S., Alessi D.S., Bolan N.S., Wu X.L., Zhang Y., Jiang X.D., Tu Z.H., Wang H.L., Effect of fulvic acid co-precipitation on biosynthesis of Fe(III) hydroxysulfate and its adsorption of lead, Environ. Pollut., 295, (2022)
  • [3] Boland D.D., Collins R.N., Payne T.E., Waite T.D., Effect of amorphous Fe(III) oxide transformation on the Fe(II)-mediated reduction of U(VI), Environ. Sci. Technol., 45, pp. 1327-1333, (2011)
  • [4] Boland D.D., Collins R.N., Glover C.J., Payne T.E., Waite T.D., Reduction of U(VI) by Fe(II) during the Fe(II)-Accelerated transformation of ferrihydrite, Environ. Sci. Technol., 48, pp. 9086-9093, (2014)
  • [5] Boye K., Noel V., Tfaily M.M., Bone S.E., Williams K.H., Bargar J.R., Fendorf S., Thermodynamically controlled preservation of organic carbon in floodplains, Nat. Geosci., 10, pp. 415-419, (2017)
  • [6] Chen C., Kukkadapu R., Sparks D.L., Influence of coprecipitated organic matter on Fe<sup>2+</sup>(aq)-catalyzed transformation of ferrihydrite: implications for carbon dynamics, Environ. Sci. Technol., 49, pp. 10927-10936, (2015)
  • [7] Chen Y.X., Jiang X.S., Wang Y., Zhuang D.F., Spatial characteristics of heavy metal pollution and the potential ecological risk of a typical mining area: a case study in China, Process Saf. Environ., 113, pp. 204-219, (2018)
  • [8] Chen L., Yang J.Y., Wang D., Phytoremediation of uranium and cadmium contaminated soils by sunflower (Helianthus annuus L.) enhanced with biodegradable chelating agents, J. Clean. Prod., 263, (2020)
  • [9] Chen L., Wang J.Z., Beiyuan J., Guo X.T., Wu H., Fang L.C., Environmental and health risk assessment of potentially toxic trace elements in soils near uranium (U) mines: a global meta-analysis, Sci. Total Environ., 816, (2022)
  • [10] Coward E.K., Ohno T., Sparks D.L., Direct evidence for temporal molecular fractionation of dissolved organic matter at the iron oxyhydroxide interface, Environ. Sci. Technol., 53, pp. 642-650, (2019)