Diffusion coefficients of polar organic compounds in agarose hydrogel and water and their use for estimating uptake in passive samplers
Language English Country England, Great Britain Media print-electronic
Document type Journal Article
PubMed
32088466
DOI
10.1016/j.chemosphere.2020.126183
PII: S0045-6535(20)30376-3
Knihovny.cz E-resources
- Keywords
- Agarose hydrogel, DGT, Diffusion coefficient, Passive sampling, Polar organic compounds, Taylor dispersion,
- MeSH
- Biological Transport MeSH
- Water Pollutants, Chemical analysis MeSH
- Diffusion MeSH
- Hydrogels MeSH
- Kinetics MeSH
- Cosmetics MeSH
- Environmental Monitoring instrumentation methods MeSH
- Organic Chemicals MeSH
- Pesticides analysis MeSH
- Sepharose analysis MeSH
- Temperature MeSH
- Water MeSH
- Publication type
- Journal Article MeSH
- Names of Substances
- Water Pollutants, Chemical MeSH
- Hydrogels MeSH
- Cosmetics MeSH
- Organic Chemicals MeSH
- Pesticides MeSH
- Sepharose MeSH
- Water MeSH
Diffusion coefficient (D) is an important parameter for prediction of micropollutant uptake kinetics in passive samplers. Passive samplers are nowadays commonly used for monitoring trace organic pollutants in different environmental matrices. Samplers utilising a hydrogel layer to control compound diffusion are gaining popularity. In this work we investigated diffusion of several perfluoroalkyl substances, currently used pesticides, pharmaceuticals and personal care products in 1.5% agarose hydrogel by measuring diffusion coefficients using two methods: a diffusion cell and a sheet stacking technique. Further, diffusion coefficients in water were measured using Taylor dispersion method. The sheet stacking method was used to measure D at 5, 12, 24, and 33 °C in order to investigate temperature effect on diffusion. Median D values ranged from 2.0 to 8.6 × 10-6 cm2 s-1 and from 2.1 to 8.5 × 10-6 cm2 s-1 for the diffusion cell and sheet stack methods respectively. For most compounds, the variability between replicates was higher than the difference between values obtained by the two methods. Rising temperature from 10 to 20 °C increases the diffusion rate by the factor of 1.41 ± 0.10 in average. In water, average D values ranged from 3.03 to 10.0 × 10-6 cm2 s-1 and were comparable to values in hydrogel, but some compounds including perfluoroalkyl substances with a long aliphatic chain could not be evaluated properly due to sorptive interactions with capillary walls in the Taylor dispersion method. Sampling rates estimated using the measured D values were systematically higher than values estimated from laboratory sampler calibration in our previously published study, by the factor of 2.2 ± 1.0 in average.
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