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Effect of long-term electrodialytic soil remediation on Pb removal and soil weathering.

Author(s): Skibsted G, Ottosen LM, Elektorowicz M, Jensen PE

J Hazard Mater. 2018 Sep 15;358:459-466 Authors: Skibsted G, Ottosen LM, Elektorowicz M, Jensen PE

Article GUID: 29801718


Title:Effect of long-term electrodialytic soil remediation on Pb removal and soil weathering.
Authors:Skibsted GOttosen LMElektorowicz MJensen PE
Link:https://www.ncbi.nlm.nih.gov/pubmed/29801718?dopt=Abstract
Category:J Hazard Mater
PMID:29801718
Dept Affiliation: ENCS
1 Department of Civil Engineering, Technical University of Denmark, Building 118, 2800 Kgs. Lyngby, Denmark.
2 Department of Building, Civil and Environmental Engineering, Concordia University, Montreal, Quebec, Canada.
3 Department of Civil Engineering, Technical University of Denmark, Building 118, 2800 Kgs. Lyngby, Denmark. Electronic address: pej@byg.dtu.dk.

Description:

Effect of long-term electrodialytic soil remediation on Pb removal and soil weathering.

J Hazard Mater. 2018 Sep 15;358:459-466

Authors: Skibsted G, Ottosen LM, Elektorowicz M, Jensen PE

Abstract

Weathering of soil minerals during long-term electrochemical soil remediation was evaluated for two different soils: an industrially Pb contaminated soil with high carbonate content and an unpolluted soil with low carbonate content. A constant current of 5?mA was applied for 842 days, and sampling was made 22 times during the treatment. The overall qualitative mineral composition was unaffected by electrodialysis, except for calcite removal which was complete. However, dissolution and removal of Al, Fe, Si, Mg, Ca and Pb from the soil during the treatment exceeded the fraction extractable by digestion in 7?M HNO3, and provided evidence of enhanced mineral dissolution induced by the current. Nevertheless, the total dissolved Si and Al only constituted 0.2-0.3% and 1.1-3.5% of the total content, while the Pb overall removal from the contaminated soil was only 8.1%. An observed reduction in the dry matter of 4.5% and 13.5% from the two soils, respectively was mainly due to dissolution of CaCO3 and organic matter, but also included a minor dissolution of other soil minerals.

PMID: 29801718 [PubMed - in process]