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Removal of Arsenic Using a Cationic Polymer Gel Impregnated with Iron Hydroxide
Published on: June 28, 2019
Arsenic-bicarbonate interaction on goethite particles.
Monika Stachowicz1, Tjisse Hiemstra, Willem H van Riemsdijk
1Department of Soil Quality, Wageningen University, PO Box 47, 6700 AA Wageningen, The Netherlands.
Dissolved bicarbonate competes with arsenic (arsenate and arsenite) for binding sites on goethite, especially at lower pH. This competition is less significant than other factors like phosphate in natural arsenic contamination.
Area of Science:
- Environmental Chemistry
- Geochemistry
- Water-Rock Interaction
Background:
- Arsenic contamination in groundwater is a significant environmental and health concern.
- Understanding the adsorption mechanisms of arsenic species on mineral surfaces is crucial for remediation.
- Bicarbonate is a common component in natural waters and its role in arsenic adsorption requires investigation.
Purpose of the Study:
- To investigate the competitive interaction between bicarbonate and arsenic (As(V) and As(III)) on goethite.
- To model these interactions using the charge distribution (CD) model.
- To assess the significance of bicarbonate competition in natural arsenic-contaminated systems.
Main Methods:
- Batch adsorption experiments were conducted using goethite under environmentally relevant pH and arsenic concentrations.
- Single ion adsorption data for bicarbonate, As(III), and As(V) were used to parameterize the CD model.
- The CD model was applied to predict the competitive effects of bicarbonate on arsenic adsorption.
Main Results:
- Dissolved bicarbonate was found to compete with both As(V) and As(III) for adsorption sites on goethite.
- The competitive effect of bicarbonate was most pronounced at lower pH values (around 6.5).
- The CD model successfully predicted the competitive behavior of bicarbonate.
Conclusions:
- Bicarbonate is a competing ligand for arsenic adsorption on goethite, particularly at circumneutral pH.
- The calculated natural arsenic loading on aquifer materials suggests that bicarbonate competition alone cannot explain arsenic levels.
- Other strong competitors, such as phosphate and natural organic matter, likely play a more dominant role in controlling arsenic concentrations in natural systems.
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