期刊
CHEMICAL ENGINEERING JOURNAL
卷 172, 期 2-3, 页码 689-697出版社
ELSEVIER SCIENCE SA
DOI: 10.1016/j.cej.2011.06.036
关键词
Chelating agent; Fenton-like; Hydrogen peroxide; ISCO; Stabilizer
资金
- Comunidad Autonoma de Madrid [S2009AMB-1648]
- Spanish Ministry of Science and Innovation [CTM2006-00317, CTM2010-16693]
In situ chemical oxidation (ISCO) is a powerful technology for soil remediation. However, one of the main drawbacks of an in situ Fenton-like treatment (H(2)O(2) + natural Fe species present in soil) relies in the instability of H(2)O(2) when is in contact with soil. Besides, organic pollutants can be strongly entrapped on the soil organic matter (SUM) diminishing the efficiency of the ISCO technology. The H(2)O(2) stabilization was evaluated, in this work, using KH(2)PO(4) and six different chelating agents (EDTA, L-ascorbic acid, gallic acid, citric acid, sodium citrate mono-hydrate (CITRm), sodium citrate 2-hydrate (CITRm), at different experimental conditions, in three different calcareous loamy sand soils, with different SOM, iron and manganese amounts. A negligible stabilization effect is noticed using KH(2)PO(4) in soils with the highest SOM content, probably due to SOM coating the iron and manganese minerals. EDTA did not produce any relevant effect on the H(2)O(2) decomposition in neither of the soils analyzed. A certain decrease of the hydrogen peroxide conversion was observed for the L-ascorbic, gallic and citric acids. While CITRm and CITRt produced a significant stabilization effect of H(2)O(2). Higher efficiencies are obtained with CITRm due to the acidification of the soils produced by chelating agent. The influence of the chelating agent addition on remediation of soil contaminated with 2,4-dimethylphenol (2,4-DMP) was also analyzed. The addition of EDTA or CITRt as chelating agents produced an increase of the 2,4-DMP degradation. This could be explained because chelating agents stabilize the hydrogen peroxide, enhance desorption of the entrapped pollutant and solubilize part of the iron from the soil. (C) 2011 Elsevier B.V. All rights reserved.
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