2020
DOI: 10.1016/j.watres.2020.115685
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Importance of Al/Fe oxyhydroxide coating and ionic strength in perfluorooctanoic acid (PFOA) transport in saturated porous media

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Cited by 41 publications
(20 citation statements)
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“…The zeta potentials of different sand at pH from 4.5 to 9.7 followed the order of Al-3 (− 19.9 ~ 42. 2), consistent with previous findings (Lyu et al, 2020;Wang et al, 2012). This is likely due to the great disparity in pH PZC (point of zero charge), which followed the order of Al oxyhydroxide (9.9; Figure S3) > Fe oxyhydroxide (7.2; Figure S3) > quartz sand (2-3) (Fisher-Power & Cheng, 2018).…”
Section: Characteristics Of Psnp Suspension and Sandsupporting
confidence: 90%
See 1 more Smart Citation
“…The zeta potentials of different sand at pH from 4.5 to 9.7 followed the order of Al-3 (− 19.9 ~ 42. 2), consistent with previous findings (Lyu et al, 2020;Wang et al, 2012). This is likely due to the great disparity in pH PZC (point of zero charge), which followed the order of Al oxyhydroxide (9.9; Figure S3) > Fe oxyhydroxide (7.2; Figure S3) > quartz sand (2-3) (Fisher-Power & Cheng, 2018).…”
Section: Characteristics Of Psnp Suspension and Sandsupporting
confidence: 90%
“…The sand was cleaned using a procedure described previously (Tian et al, 2010). A fraction of cleaned sand (referred to uncoated sand, Un) was coated with different concentrations of Fe/Al oxyhydroxide following methods reported in previous studies (detailed in S1) (Kuan et al, 1998;Lyu et al, 2020;Stahl & James, 1991;Wang et al, 2013). The sand coated with three concentration gradients (low, medium, high) of Fe/Al oxyhydroxide is designated as Fe-1 and Al-1 (low), Fe-2 and Al-2 (medium), and Fe-3 and Al-3 (high), respectively.…”
Section: Porous Mediamentioning
confidence: 99%
“…As summarized in recent critical reviews, , retardation of nonpolymeric PFAS within vadose zone soils is a complex combination of multiple retention mechanisms and processes. Specific to the anionic perfluoroalkyl acids (PFAAs) of primary regulatory interest relevant to legacy AFFF formulations, these include hydrophobic interactions with the organic carbon (OC) fraction in soil, electrostatic interactions with the surfaces of variable-charged clay minerals including iron (Fe) and aluminum (Al) oxides and hydroxides to include potential irreversible chemisorption, and fluid–fluid (e.g., air–water) interfacial accumulation resulting in retardation from a “surface excess”. Laboratory experiments further suggest that PFAA transport in soil is complicated by rate-limiting kinetics attributable to diffusive fluxes into and out of the OC matrix and associated hydrophobic solid-phase interactions, nonlinear (i.e., concentration-dependent) sorption to both solids and air–water interfaces, , and significant desorption hysteresis resulting at least in part from biphasic porosity domains (highlighting the importance of diffusive fluxes) within natural soils. , In general, PFAS transport through unsaturated soil is “nonideal” even at environmentally relevant concentrations, and studies have suggested that kinetic models with these multiprocess retention mechanisms may be prerequisites for simulating transport under field conditions. , The various soil retention processes and their kinetics, interactions thereof, and potential confounding effects from the accumulation of PFAAs in soil as a result of polyfluorinated precursor transformation are the subject of much ongoing research …”
mentioning
confidence: 99%
“…Li et al, 2019;Sima & Jaffé, 2021;Wei et al, 2017). However, it has been demonstrated that other soil constituents such as metal oxides and clay minerals can also contribute to PFAS sorption, particularly for shorter-chain PFAS and soils with lower SOM contents (Higgins & Luthy, 2006;Lyu et al, 2020;Pereira et al, 2018;Wang et al, 2021). PFAS sorption has in some cases been observed to be a function of pH, ionic strength, and the degree of ionization of the PFAS.…”
Section: Soil Retentionmentioning
confidence: 99%