Modeling Pb(II) adsorption onto sandy loam soil.
1Department of Civil Engineering, I-Shou University, Da-Shu Shiang, Kaohsiung County 84008, Taiwan. chweng@isu.edu.tw
Journal of Colloid and Interface Science
|March 19, 2004
Summary
This study shows that lead (Pb(II)) adsorption on sandy loam soil increases with pH and surface loading. Specific chemical interactions, not just physical binding, are key to lead removal from soil.
Area of Science:
- Environmental Science
- Soil Science
- Geochemistry
Background:
- Lead (Pb(II)) is a toxic heavy metal pollutant.
- Soil contamination by heavy metals poses risks to ecosystems and human health.
- Understanding lead adsorption mechanisms in soil is crucial for remediation strategies.
Purpose of the Study:
- To investigate the adsorption behavior of Pb(II) onto hydrous sandy loam soil.
- To determine the influence of pH and surface loading on Pb(II) adsorption.
- To elucidate the surface acidity of the soil and model the adsorption process.
Main Methods:
- Batch equilibrium adsorption experiments were conducted.
- Electrophoretic mobility measurements were used to determine soil surface acidity.
- A surface complex formation model (SCFM) was applied to analyze adsorption data.
Main Results:
- Pb(II) adsorption increased with rising pH and surface loading.
- Soil surface acidity constants (pK(a1)(int) = 1.57, pK(a2)(int) = 3.43) were determined.
- Adsorption free energies for Pb2+ and Pb(OH)+ ions ranged from -5.74 to -10.00 kcal/mol.
- Specific chemical interactions were identified as the primary adsorption mechanism.
Conclusions:
- Hydrous sandy loam soil effectively adsorbs Pb(II), with adsorption enhanced by higher pH and loading.
- Surface complexation modeling accurately describes Pb(II) adsorption, highlighting the role of soil surface hydroxyl groups.
- The findings indicate that chemical interactions are dominant in lead sequestration by this soil type, informing soil remediation efforts.
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