2015
DOI: 10.1016/j.chemosphere.2015.03.024
|View full text |Cite
|
Sign up to set email alerts
|

Influence of cations on the partition behavior of perfluoroheptanoate (PFHpA) and perfluorohexanesulfonate (PFHxS) on wastewater sludge

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
10
0

Year Published

2016
2016
2024
2024

Publication Types

Select...
6
3

Relationship

0
9

Authors

Journals

citations
Cited by 51 publications
(10 citation statements)
references
References 30 publications
0
10
0
Order By: Relevance
“…Log transformations of both K d and organic carbon did not improve correlations (Table S13). At the lowest levels of organic carbon (0.098–0.12%), the K d ( C w i = 110 nM) values for the 6:2 and 8:2 FtS are similar in magnitude to those for the soils with higher organic carbon (1.0–2.3%), which indicates that the mineral phase in the low-organic-carbon soils (Soils 2 and 6) influences sorption. , The nonpolar fluorinated tail of the anionic FtSs may interact with the hydrophobic (nonpolar) nanosites between the charged sites on the mineral surface via weak hydrophobic interactions. , …”
Section: Resultsmentioning
confidence: 81%
See 1 more Smart Citation
“…Log transformations of both K d and organic carbon did not improve correlations (Table S13). At the lowest levels of organic carbon (0.098–0.12%), the K d ( C w i = 110 nM) values for the 6:2 and 8:2 FtS are similar in magnitude to those for the soils with higher organic carbon (1.0–2.3%), which indicates that the mineral phase in the low-organic-carbon soils (Soils 2 and 6) influences sorption. , The nonpolar fluorinated tail of the anionic FtSs may interact with the hydrophobic (nonpolar) nanosites between the charged sites on the mineral surface via weak hydrophobic interactions. , …”
Section: Resultsmentioning
confidence: 81%
“…14,17 The nonpolar fluorinated tail of the anionic FtSs may interact with the hydrophobic (nonpolar) nanosites 51−54 between the charged sites on the mineral surface 55 via weak hydrophobic interactions. [14][15][16]56 The lack of a correlation in FtS sorption may be due to variations in the extent of organic matter decomposition of the soils tested. The relationship between C and N in soil organic matter and oxygen-containing functional groups is based on the following two premises: (a) the majority of terrestrial organic matter is decomposed by oxidative depolymerization, 57 which adds oxygen-containing functional groups to oxidized compounds, 58 and (b) oxidative depolymerization of faunal debris (C/N > 25) is carried out by microbiota (C/N = 6−10), in which "fresh" organic debris with a large C/N ratio (i.e., 30) are slowly converted into an amorphous heterogeneous organic phase (humic substances) with a small C/N ratio (i.e., 12).…”
Section: Sorption Isotherms Sorption Experiments With Nationalmentioning
confidence: 99%
“…Organic characteristics of solids were demonstrated to be crucial to the sorption of PFAS (Wang et al 2015a). The authors determined that an activated sludge with a higher content of biological organics had greater affinity than primary treatment solids for PFAS.…”
Section: Residual Solidsmentioning
confidence: 99%
“…Among replacements of long-chain PFASs used currently by the industry, there are short-chain PFASs (C4-C6), including perfluorohexane acid (PFHxA) or perfluorobutane sulfonic acid (PFBS). Some reports have indicated a higher environmental mobility of short-chain PFASs, compared to their long-chain equivalents [21]. It has been revealed that biochemical PFHxS half-life in the human blood (young females) is longer than that of PFOS [22,23].…”
Section: Long-chain Pfass Alternativesmentioning
confidence: 99%