Back to Search
Start Over
Transformation of dissolved organic matter during groundwater arsenite removal using air cathode iron electrocoagulation.
- Source :
-
Chemosphere . Jun2024, Vol. 358, pN.PAG-N.PAG. 1p. - Publication Year :
- 2024
-
Abstract
- Dissolve organic matters (DOM) usually showed negative effect on the removal of inorganic arsenic (As) in groundwater by electrochemical approaches, yet which parts of sub-component within DOM played the role was lack of evidence. Herein, we investigated the effects of land-source humic-like acid (HA) on groundwater As(III) removal using air cathode iron electrocoagulation, based on the parallel factor analysis of three-dimensional excitation–emission matrix and statistical methods. Our results showed that the land-source HA contained five kinds of components and all components presented significantly negative correlations with the removal of both As(III) and As(V). However, the high aromatic fulvic-like acid and low aromatic humic-like acid components of land-source HA presented the opposite correlations with the concentration of As(III) during the reaction. The high aromaticity fulvic-like components of land-source HA (Sigma-Aldrich HA, SAHA) produced during the reaction facilitated the oxidation of As(III) due to its high electron transfer capacities and good solubility in wide pH range, but the low aromaticity humic-like ones worked against the oxidation of As(III). Our findings offered the novel insights for the flexible activities of DOM in electron Fenton system. [Display omitted] • Humic acid presented negative correlations with the removal of both As(III) and As(V). • High aromatic fulvic-like acid facilitated the oxidation of As(III). • Electron transfer capacities of humic substance had flexible effects on As(III) removal. [ABSTRACT FROM AUTHOR]
Details
- Language :
- English
- ISSN :
- 00456535
- Volume :
- 358
- Database :
- Academic Search Index
- Journal :
- Chemosphere
- Publication Type :
- Academic Journal
- Accession number :
- 177248187
- Full Text :
- https://doi.org/10.1016/j.chemosphere.2024.142083