4.7 Article

Experimental and computational study on the inhibitory effect of phytic acid on U(VI) biomineralization by Shewanella putrefaciens

Journal

CHEMICAL ENGINEERING JOURNAL
Volume 450, Issue -, Pages -

Publisher

ELSEVIER SCIENCE SA
DOI: 10.1016/j.cej.2022.138364

Keywords

Shewanella putrefaciens; U(VI); Phytic acid; Quantum -theoretical modeling; Biomineralization

Funding

  1. National Natural Science Foundation of China [41877323, 22033005]
  2. Guangdong Provincial Key Laboratory of Catalysis [2020B121201002]
  3. NHC Key Laboratory of Nuclear Technology Medical Transformation [2021HYX004]

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The study investigates the role of phytic acid on U(VI) biomineralization and reveals its inhibition effect on U(VI) removal by Shewanella putre-faciens. Phytic acid tends to chelate with U(VI) to form colloid polymer. Calcium and magnesium ions can bind with phytic acid, relieving its inhibition effect. The bacteria mainly interact with U(VI) through phosphorous functional groups.
Uranyl (UO22+) species with hexavalent U(VI) oxidation state is the most ubiquitous form of uranium in natural minerals, underground water, contaminated soils, and ocean. Interplay between bioorganic molecules and U(VI) is rather complicated due to its various complex configurations and reaction networks. In this study, the widely present phytic acid (IP6) is selected as a model organic molecule together with the bacteria Shewanella putre-faciens (S. putrefaciens, existing mainly in marine environments) to explore its role on U(VI) biomineralization. We found that phytic acid had a clear inhibition effect on the U(VI) removal of S. putrefaciens, with the absorption capacity dropped from 382.77 mg/g to 102.45 mg/g. Further Dialysis experiment suggested that phytic acid tended to chelate with U(VI) to form colloid polymer. Quantum-theoretical modeling confirmed that phytic acid bond strongly with uranyl ions, while calcium and magnesium ions could bind with phytic acid as well via ionic bonding, thus relieving the inhibition effect of phytic acid in the solution through breaking the hydrogen bonding network. XRD and SEM-EDS results showed that phytic acid could hinder the formation of mineralized body (Metanatroautunite [Na(UO2)(PO4).3H(2)O]) and prefer to form amorphous material. Further FTIR and XPS data illustrated that the bacteria mainly interacted with U(VI) through phosphorous functional groups. This study presents detailed information for colloid formation between phytic acid and U(VI) as well as the critical role of Ca2+ and Mg2+ ions on the matrix of S. putrefaciens bacteria, combining with molecular-level microscopic un-derstanding on the chemical behavior of U(VI) in the presence of inorganic and organic ions in soil and water.

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