Cited by 26Per- and polyfluoroalkyl substances researchGroundwater flow and contamination studiesSoil and Unsaturated Flow

Numerical modeling of PFAS movement through the vadose zone: Influence of plant water uptake and soil organic carbon distribution

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Biesek, Barbara Jennifer, Szymkiewicz, Adam, Šimůnek, Jirka, Gumuła-Kawęcka, Anna, Jaworska-Szulc, Beata·2024·Science of The Total Environment

Abstract

In this study, we investigated the effects of soil organic carbon (SOC) distribution and water uptake by plant roots on PFAS movement in the vadose zone with a deep groundwater table under temperate, humid climate conditions. Two series of numerical simulations were performed with the HYDRUS computer code, representing the leaching of historical PFOS contamination and the infiltration of water contaminated with PFOA, respectively. We considered soil profiles with three distributions of SOC (no SOC, realistic SOC distribution decreasing with depth, and uniform SOC equal to the content measured in topsoil), three root distributions (bare soil, grassland, and forest), and three soil textures (sand, sandy loam, and loam). The SOC distribution had a profound impact on the velocity of PFOS movement. The apparent retardation factor for realistic SOC distribution was twice as large as for the scenario with no SOC and more than three times smaller than for the scenario with uniformly high SOC content. We also showed that the root distribution in soil profoundly impacts the simulations of PFAS migration through soil. Including the root zone significantly slows down the movement of PFAS, primarily due to increased evapotranspiration and reduced downward water flux. Another effect of water uptake by plant roots is an increase of PFAS concentrations in soil water (evapo-concentration). The evapo-concentration and the slowdown of PFAS movement due to root water uptake are more significant in fine-textured soils than in sand.

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Crossref · 10.1016/j.scitotenv.2024.173252

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  • Short-chain PFASs are more water-soluble, less strongly retained, and thus more mobile and more likely to be taken up and translocated by plants.

    “In contrast, short-chain PFASs are more water-soluble, less strongly retained, and thus more mobile and more likely to be taken up and translocated by plants [162-164].”
  • Soil organic carbon content slows PFAS movement by increasing sorption, especially for long-chain PFASs, which bind more strongly to soil and are less mobile.

    “Soil organic carbon (SOC) content slows PFAS movement by increasing sorption, especially for long-chain PFASs, which bind more strongly to soil and are less mobile.”

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Authors
Biesek, B. J., Szymkiewicz, A., Šimůnek, J., Gumuła-Kawęcka, A., & Jaworska-Szulc, B.
Affiliations
Gdańsk University of Technology (PL)
Corresponding author
Biesek, Barbara Jennifer
Venue
Science of The Total Environment
Publisher
Elsevier BV
Published
2024-07
Volume
935
Pages
173252
ISSN
0048-9697 (ISSN-L)
OpenAlex
W4397032545
Cited by
26
References
38
Citations by year
2026: 14 · 2025: 11 · 2024: 1
FWCI
3.43
Type
journal article
Language
en
Open access
Locations
  • The Science of The Total Environment (publishedVersion, cc-by-nc-nd)
  • PubMed (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Environmental Chemistry › Per- and polyfluoroalkyl substances research
  • Physical Sciences › Environmental Science › Environmental Engineering › Groundwater flow and contamination studies
  • Physical Sciences › Engineering › Civil and Structural Engineering › Soil and Unsaturated Flow
Keywords
PFAS, PFOS, perfluorooctanoic acid, vadose zone, soil organic carbon distribution, root water uptake, evapotranspiration, contaminant leaching, infiltration, soil texture

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