Effects of dissolved organic carbon on desorption of aged phenanthrene from contaminated soils: A mechanistic study.

Environ Pollut

State Key Laboratory of Environmental Chemistry and Ecotoxicology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.

Published: November 2019

AI Article Synopsis

  • Dissolved organic carbon (DOC) significantly impacts the sorption/desorption and transportation of hydrophobic organic contaminants (HOCs) in soil, but the exact mechanisms, especially regarding aged contaminants, are not well understood.
  • In experiments with DOC from different sources and oxalate, it was found that desorption of aged phenanthrene was mainly influenced by soil organic carbon content and that the presence of DOC in solutions enhanced phenanthrene desorption compared to just water.
  • The study also revealed that the molecular composition of DOC plays a critical role in facilitating phenanthrene desorption, highlighting specific interactions between DOC and phenanthrene that could inform better environmental management of contaminated soils.

Article Abstract

Dissolved organic carbon (DOC) has a major influence upon sorption/desorption and transport of hydrophobic organic contaminants (HOCs) in soil environments. However, the molecular mechanisms of DOC sorption and its effects on aged HOC desorption in contaminated soils still remain largely unclear. Here, effects of three different DOC (one from commercial peat and two from biochars produced at 300 °C and 500 °C pyrolysis temperatures, respectively) and oxalate (as a reference) on abiotic desorption behavior of aged phenanthrene from three agricultural soils were investigated. Results showed that desorption of aged phenanthrene from soils was predominantly dependent on soil organic carbon content. The presence of DOC and oxalate resulted in higher desorption of phenanthrene compared to water alone, and the effects were positively related to soil organic carbon content and DOC/oxalate concentration. The facilitating effects of DOC were further increased during the second consecutive desorption, whereas oxalate had no such effect. Ultra-high-resolution Fourier transform-ion cyclotron resonance-mass spectrometry confirmed the molecular fractionation of DOC at the soil-water interface during DOC sorption. Specifically, the DOC molecules with O-rich moieties were preferentially adsorbed, whereas the molecules with phenolic and aromatic structures were selectively retained in the soil solutions through competitive displacement and co-sorption reactions during sorption. The enriched phenyl structures in the retained DOC facilitated its association with phenanthrene in the solutions and thus the release of phenanthrene from the soils. In contrast, oxalate replaced some organic carbon from the soils and thus released the associated phenanthrene into the solutions. Our findings highlight the importance of the molecular composition and structure of DOC for the desorption of phenanthrene in soil-water environments, which may help improve our understanding of the release and transport of organic compounds in the environments.

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http://dx.doi.org/10.1016/j.envpol.2019.113016DOI Listing

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