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Sediment-associated reactions of aromatic amines. 2. QSAR development
Dalizza Colón1, Eric J Weber, George L Baughman
1National Exposure Research Laboratory, U.S. Environmental Protection Agency, Athens, Georgia 30605, USA.
Aromatic amines bind irreversibly in soils and sediments. Dissociation constants and Hammett sigma constants best predict the reaction rates of substituted anilines, guiding environmental fate assessments.
Area of Science:
- Environmental Chemistry
- Soil Science
- Organic Geochemistry
Background:
- Aromatic amines are common in organic chemicals, but their environmental fate, particularly binding kinetics in soils and sediments, is not fully understood.
- Irreversible binding via nucleophilic addition and oxidative radical coupling dominates aromatic amine fate.
- Predicting reaction kinetics in natural systems requires understanding molecular properties influencing sorption.
Purpose of the Study:
- To investigate the sorption kinetics of substituted anilines in sediment slurries.
- To identify molecular descriptors that correlate with and predict the reaction rates of aromatic amines.
- To differentiate between factors controlling rapid and slow sorption processes.
Main Methods:
- Measured sorption kinetics of various anilines with ortho, meta, and para substituents in sediment slurries.
- Characterized sorption kinetics into rapid and slow phases.
- Correlated initial sorption rates with molecular descriptors like pKa, Hammett sigma constants, and redox potentials.
Main Results:
- Sorption kinetics exhibited an initial rapid phase followed by a slower phase.
- Initial sorption rates were influenced by the type and position of aniline substituents.
- Dissociation constants (pKa) and Hammett sigma constants showed the strongest linear correlations with initial reaction rates.
Conclusions:
- Dissociation constants and Hammett sigma constants are valuable for predicting substituted aniline reaction rates in sediments.
- The slow sorption phase is less sensitive to substituent effects, suggesting it's limited by binding site availability rather than electron transfer rates.
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