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Concentration-dependent kinetics of pollutant desorption from soils.
Washington J Braida1, Jason C White, Dongye Zhao
1The Connecticut Agricultural Experiment Station, 123 Huntington Street, P.O. Box 1106, New Haven, Connecticut 06504-1106, USA.
Environmental Toxicology and Chemistry
|December 5, 2002
Summary
Soil pollutant desorption rates increase with initial concentration, but a resistant fraction remains. This highlights the importance of considering contaminant concentration in soil transport and bioavailability studies.
Area of Science:
- Environmental Science
- Soil Science
- Chemical Engineering
Background:
- Sorption-desorption kinetics are crucial for understanding pollutant transport and bioavailability in soils.
- Contaminant concentration is a key factor influencing these kinetics.
- Previous research examined concentration effects on uptake rates.
Purpose of the Study:
- To investigate the impact of initial phenanthrene sorbed concentration (q(0)) on desorption rates from six soils.
- To analyze the formation and characteristics of a highly resistant fraction during desorption.
- To evaluate the applicability of the dual-mode diffusion model (DMDM) to desorption kinetics.
Main Methods:
- Soils were pre-equilibrated with phenanthrene for 180 days.
- Desorption rates were measured using a polymer adsorbent (Tenax) as a third-phase sink.
- Empirical curve fitting and the dual-mode diffusion model (DMDM) were applied to analyze kinetic data.
Main Results:
- Fractional desorption rates increased with initial sorbed concentration (q(0)) for nonlinear isotherms.
- A highly resistant fraction (4-31% of q(0)) persisted after long-term desorption.
- The resistant fraction decreased with increasing q(0) for nonlinear isotherms but increased for linear isotherms.
- The DMDM provided good fits to the nonresistant fraction, linking diffusivity to immobile sites.
Conclusions:
- Contaminant concentration significantly affects soil desorption rates and the persistence of resistant fractions.
- The dual-mode diffusion model explains concentration-dependent diffusivity through changes in sorbate site occupancy.
- Findings support heterogeneous soil organic matter models and emphasize the need to account for concentration effects in desorption studies.