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Ionic strength reduction and flow interruption enhanced colloid-facilitated Hg transport in contaminated soils
Yingjia Zhu1, Lena Q Ma2, Xiaoling Dong1
1Soil and Water Science Department, University of Florida, Gainesville, FL 32611, USA.
Reducing ionic strength and interrupting flow significantly increased colloidal mercury (Hg) release from contaminated soils. Organic matter in colloids acts as a key carrier for mercury transport.
Area of Science:
- Environmental Science
- Geochemistry
- Soil Science
Background:
- Mercury (Hg) contamination in soils poses environmental risks.
- Understanding mercury transport mechanisms is crucial for remediation.
- Colloidal particles can mobilize contaminants in soil leachate.
Purpose of the Study:
- To investigate the impact of ionic strength reduction and flow interruption on colloidal mercury release.
- To identify the role of soil organic matter and other fractions in mercury transport.
- To determine the primary carriers of mercury in leachate under altered flow conditions.
Main Methods:
- Column leaching experiments were conducted on two mercury-contaminated soils.
- Ionic strength was reduced from 5mM to 0.05mM.
- Flow interruption (7 days) was simulated; leachate was analyzed for colloidal mercury, organic matter, and iron.
Main Results:
- Both ionic strength reduction and flow interruption substantially increased colloidal mercury release (44-48% of total released Hg).
- Peak colloidal mercury concentrations (27.8 and 360 μg/L) were observed after flow interruption.
- Colloidal organic matter and iron concentrations correlated with colloidal mercury, indicating their role as carriers.
Conclusions:
- Colloidal organic matter is a significant carrier for mercury transport in soils, particularly under reduced ionic strength and flow interruption.
- Altered hydrological conditions can enhance the mobilization of mercury-bound colloids.
- Findings highlight the importance of considering colloidal transport in mercury-contaminated site assessments and management.
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