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Effects of pH, organic acids, and inorganic ions on lead desorption from soils
The desorption characteristics of lead in two variable charge soils (one developed from Arenaceous rock (RAR) and the other derived from Quaternary red earths (REQ)) were studied, and the effects of pH value, organic acid, and competitive ions were examined. Desorption of Pb 2+ decreased from nearly...
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Published in: | Environmental pollution (1987) 2006-09, Vol.143 (1), p.9-15 |
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Main Authors: | , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The desorption characteristics of lead in two variable charge soils (one developed from Arenaceous rock (RAR) and the other derived from Quaternary red earths (REQ)) were studied, and the effects of pH value, organic acid, and competitive ions were examined. Desorption of Pb
2+ decreased from nearly 100.0 to 20.0% within pH 1.0–4.0 in both soils, and then the decrease diminished at pH
>
4.0. Organic ligands at relatively low concentrations (≤10
−3
mol
L
−1) slightly inhibited Pb
2+ desorption, but enhanced Pb
2+ desorption at higher concentrations. In this study, citric acid or acetic acid at higher concentrations (>10
−3
mol
L
−1) had the greatest improvement of Pb
2+ desorption, followed by malic acid; and the smallest was oxalic acid. Desorption of the adsorbed Pb
2+ increased greatly with increasing concentrations of added Cu
2+ or Zn
2+. Applied Cu
2+ increased Pb
2+ desorption more than Zn
2+ at the same loading.
The adsorption–desorption process is a basic and important reaction in soils controlling Pb
2+ mobility and bioavailability. |
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ISSN: | 0269-7491 1873-6424 |
DOI: | 10.1016/j.envpol.2005.11.010 |