4.4 Article

Comparison of adsorption behaviors of selected endocrine-disrupting compounds in soil

Journal

JOURNAL OF ENVIRONMENTAL QUALITY
Volume 50, Issue 3, Pages 756-767

Publisher

WILEY
DOI: 10.1002/jeq2.20221

Keywords

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Funding

  1. US-Israel Binational Agricultural Research and Development Fund
  2. Agronomy Department, Iowa State University
  3. National Institute of Food and Agriculture, United States Department of Agriculture

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The adsorption characteristics and mechanisms of BPA, EE2, and 4NP vary in different soils, influenced by soil organic matter and clay content.
Bisphenol-A (BPA), 17 alpha-ethinylestradiol (EE2), and 4-nonylphenol (4NP) are endocrine-disrupting chemicals (EDCs) that are useful models for studying the potential fate and transport of EDCs in soil and water environments. Two alluvial soils with contrasting physicochemical properties were used as adsorbents for this study. The Zook soil material had more organic matter and clay than the sandy loam Hanlon soil material. Batch equilibrium experiments were performed to generate adsorption isotherms, to determine the adsorption parameters, and to assess desorption hysteresis. Adsorption of BPA to both soils followed an L-type isotherm, and 4NP adsorbed to both Hanlon and Zook soils exhibited S-shape isotherms. EE2 adsorbed to the Zook soil also followed an S-shaped isotherm, but EE2 adsorbed to the Hanlon soil showed an H-type isotherm. Overall, the Sips model fit the data well, with standard errors of prediction generally <= 6%. The adsorption affinity (K-LF) values were highest for 4NP, and BPA had the lowest hysteresis indices. The data suggest that BPA was most likely adsorbed by soil organic matter via hydrogen bonding involving its two phenolic groups. In contrast, isotherm shape, model affinity indices, lack of desorption, and molecular-scale characteristics led us to infer that 4NP was adsorbed largely by the retention of molecular clusters, perhaps in clay nanopores. Finally, the adsorption of EE2 exhibited different isotherm shapes for the two soils as well as intermediate affinity and desorption indices, suggesting that EE2 molecules could be retained both by soil organic matter and by clay.

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