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The redistribution process of As(Ⅲ) and Fe(Ⅱ) caused by As/Fe ratio, organic matter, and co-existing ions: Co-precipitation and co-oxidation.
Liu, Xin; Wang, Jiankang; He, Yongxian; Li, Junfeng; Tian, Qingyuan; Xu, Hong.
Affiliation
  • Liu X; College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi 832000, PR China.
  • Wang J; College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi 832000, PR China; Key Laboratory of Water Resources Efficient Utilization in Arid Areas, Shihezi University, Shihezi 832000, PR China. Electronic address: shuibenerban@126.com.
  • He Y; College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi 832000, PR China.
  • Li J; College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi 832000, PR China. Electronic address: ljfshz@126.com.
  • Tian Q; College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi 832000, PR China.
  • Xu H; College of Water Conservancy & Architectural Engineering, Shihezi University, Shihezi 832000, PR China.
Ecotoxicol Environ Saf ; 281: 116631, 2024 Aug.
Article in En | MEDLINE | ID: mdl-38941658
ABSTRACT
The contamination of arsenic (As) in aqueous environments has drawn widespread attention, and iron compounds may largely alter the migration ability of As. However, the stability of As(III) in Fe-As system with the intervention of organic matter (OM) remains unclear. Herein, we had explored the co-precipitation and co-oxidation processes of As-Fe system by using batch experiments combined with Fourier Transform Infrared Spectroscopy (FTIR) and X-ray Photoelectron Spectroscopy (XPS) in this research. The precipitation quantity of As(III) increased (28.85-92.41 %) when the As/Fe ratio decreased, and increased (24.20-64.20 %) with pH increased. The main active substance for oxidizing As(III) was H2O2, which was produced in the As-Fe system. FTIR and XPS revealed that As(III) was first oxidized in neutral, and then absorbed and enteredthe interior of Fe(OH)3 colloids. But under alkaline conditions, As(III) was adsorbed by Fe (Oxyhydr) oxides firstly, and then oxidized. The intervention of OM would inhibit the redistribution process of As(III) in aqueous environments. Functional groups and unsaturation of the carbon chain were the dominant factors that affected the precipitation and oxidation processes of As(III), respectively. Co-existing ions (especially PO43-) also signally affected the precipitation quantity of As(Ⅲ) in the system and, when coexisting with OM, could exacerbate this process. The influence of co-existing ions on the redistributive process of As(III) in the As-Fe system with/without OM were as follows PO43- > SO42- > mixed ions > SiO32-. Moreover, high concentration of OM and PO43- might lead to morphological alterations of As, acting as a threat to aqueous environments. In summary, the present findings were to further understand and appreciate the changes of As toxicity in the aqueous environments. Particularly, the coexistence of OM and As can potentially increase the risk to drinking water safety.
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Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Oxidation-Reduction / Arsenic / Water Pollutants, Chemical / Iron Language: En Journal: Ecotoxicol Environ Saf Year: 2024 Document type: Article

Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Oxidation-Reduction / Arsenic / Water Pollutants, Chemical / Iron Language: En Journal: Ecotoxicol Environ Saf Year: 2024 Document type: Article