In-Situ Molecular-Level
Elucidation of Organofluorine
Binding Sites in a Whole Peat Soil
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Abstract
The chemical nature of xenobiotic binding sites in soils
is of
vital importance to environmental biogeochemistry. Interactions between
xenobiotics and the naturally occurring organic constituents of soils
are strongly correlated to environmental persistence, bioaccessibility,
and ecotoxicity. Nevertheless, because of the complex structural and
chemical heterogeneity of soils, studies of these interactions are
most commonly performed indirectly, using correlative methods, fractionation,
or chemical modification. Here we identify the organic components
of an unmodified peat soil where some organofluorine xenobiotic compounds
interact using direct molecular-level methods. Using <sup>19</sup>F→<sup>1</sup>H cross-polarization magic angle spinning (CP-MAS)
nuclear magnetic resonance (NMR) spectroscopy, the <sup>19</sup>F
nuclei of organofluorine compounds are used to induce observable transverse
magnetization in the <sup>1</sup>H nuclei of organic components of
the soil with which they interact after sorption. The observed <sup>19</sup>F→<sup>1</sup>H CP-MAS spectra and dynamics are compared
to those produced using model soil organic compounds, lignin and albumin.
It is found that lignin-like components can account for the interactions
observed in this soil for heptafluoronaphthol (HFNap) while protein
structures can account for the interactions observed for perfluorooctanoic
acid (PFOA). This study employs novel comprehensive multi-phase (CMP)
NMR technology that permits the application of solution-, gel-, and
solid-state NMR experiments on intact soil samples in their swollen
state