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Interaction between Per- and Polyfluoroalkyl Substances and Dissolved Organic Matter in Soil: Molecular Variation and
Yuhang Chen1,2, Dong Cao1, Mengjie Qie1,2
1State Key Laboratory of Environmental Chemistry and Toxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.
Dissolved organic matter (DOM) influences per- and polyfluoroalkyl substances (PFAS) migration in soil. Protein-like DOM components enhance PFAS porewater partitioning, while humic-like components promote soil adsorption, revealing key interactions.
Area of Science:
- Environmental Chemistry
- Soil Science
- Organic Geochemistry
Background:
- Per- and polyfluoroalkyl substances (PFAS) are persistent environmental contaminants.
- Their migration and fate in soil are influenced by soil properties, but the role of dissolved organic matter (DOM) is understudied.
- Understanding PFAS-DOM interactions is crucial for predicting contaminant transport.
Purpose of the Study:
- To investigate the interaction between PFAS and DOM in soil-porewater systems.
- To determine how DOM composition affects PFAS partitioning and distribution in field soil.
- To explore the relationship between PFAS burden and DOM characteristics.
Main Methods:
- Analysis of PFAS and DOM composition and distribution in field soil and soil-porewater.
- Quantification of total PFAS concentrations and characterization of DOM using techniques like Fourier-transform ion cyclotron resonance mass spectrometry (FT-ICR MS).
- Statistical analysis to correlate PFAS concentrations and partitioning with DOM properties and soil organic carbon content.
Main Results:
- Significant spatial variations in PFAS concentrations (3.14–50.92 ng/g) were observed.
- Higher PFAS burdens correlated with more labile and bioavailable DOM fractions (lipid/protein/amino-like) and higher DOM chemodiversity (Shannon index).
- Short-chain PFAS were particularly associated with these DOM changes. Protein-like DOM facilitated PFAS porewater partitioning, while humic-like DOM promoted soil adsorption.
Conclusions:
- DOM composition significantly dictates PFAS partitioning between soil and porewater, overriding correlations with soil organic carbon alone.
- Specific DOM components play contrasting roles: protein-like compounds enhance mobility, while humic-like compounds increase soil retention.
- These findings provide critical insights into the environmental fate and migration mechanisms of PFAS, particularly in relation to DOM dynamics.
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