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Enhanced removal of high-As(III) from Cl(-I)-diluted SO4(-II)-rich wastewater at pH 2.3 via mixed tooeleite and (Cl(-I)-free) ferric arsenite hydroxychloride formation.

Authors :
Yuan, Zidan
Zhang, Guoqing
Wu, Xing
Ma, Xu
Lin, Jinru
Wang, Shaofeng
Jia, Yongfeng
Source :
Journal of Environmental Sciences (Elsevier). Feb2023, Vol. 124, p31-41. 11p.
Publication Year :
2023

Abstract

• No precipitation of As(III) with Fe(III) in aqueous SO 4 (-II)-rich media is observed. • Mixing Cl(-I) into SO 4 (-II) solution markedly promotes As(III) precipitated removal. • The optimal As(III) removal occurs at SO 4 (-II)/Cl(-I) molar ratio of 1:4 and 25 °C. • Tooeleite and (Cl(-I)-free) ferric arsenite hydroxychloride are the main As sink. • Fe(III)-As(III) precipitate is affected by FeH 2 AsO 3 2+, FeSO 4 + and FeCl2+ complexes. An advanced cost-saving method of removal of high-As(III) from SO 4 (-II)-rich metallurgical wastewater has been developed by diluting the SO 4 (-II) content with As(III)-Cl(-I)-rich metallurgical wastewater and then by the direct precipitation of As(III) with Fe(III) at pH 2.3. As(III) removal at various SO 4 (-II)/Cl(-I) molar ratios and temperatures was investigated. The results showed that 65.2‒98.2% of As(III) immobilization into solids occurred at the SO 4 (-II)/Cl(-I) molar ratios of 1:1‒32 and 15‒60 °C in 3 days, which were far higher than those in aqueous sole SO 4 (-II) or Cl(-I) media at the equimolar SO 4 (-II) or Cl(-I) and the same temperature. SO 4 (-II)/Cl(-I) molar ratio of 1:4 and 25 °C were optimal conditions to reach the As removal maximum. Mixed aqueous SO 4 (-II) and Cl(-I) played a synergetic role in the main tooeleite formation together with (Cl(-I)-free) ferric arsenite hydroxychloride (FAHC) involving the substitution of AsO 3 3− for Cl(-I) for enhanced As fixation. The competitive complexation among FeH 2 AsO 3 2+, FeSO 4 + and FeCl2+ complexes was the main mechanism for the maximum As(III) precipitation at the SO 4 (-II)/Cl(-I) molar ratio of 1:4. Low As(III) immobilization at high temperature with increased Fe(III) hydrolysis was due to the formation of As(III)-bearing ferrihydrite with the relatively high Fe/As molar ratio at acidic pH. [Display omitted] [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
10010742
Volume :
124
Database :
Academic Search Index
Journal :
Journal of Environmental Sciences (Elsevier)
Publication Type :
Academic Journal
Accession number :
159384182
Full Text :
https://doi.org/10.1016/j.jes.2021.10.025