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Gas-particle partitioning of PCDD/Fs in daily air samples.

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Gas-particle partitioning of PCDD/Fs in daily air samples. / Lohmann, Rainer; Lee, Robert G. M.; Green, Nicholas J. L. et al.
In: Atmospheric Environment, Vol. 34, No. 16, 2000, p. 2529-2537.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Lohmann, R, Lee, RGM, Green, NJL & Jones, KC 2000, 'Gas-particle partitioning of PCDD/Fs in daily air samples.', Atmospheric Environment, vol. 34, no. 16, pp. 2529-2537. https://doi.org/10.1016/S1352-2310(99)00515-4

APA

Lohmann, R., Lee, R. G. M., Green, N. J. L., & Jones, K. C. (2000). Gas-particle partitioning of PCDD/Fs in daily air samples. Atmospheric Environment, 34(16), 2529-2537. https://doi.org/10.1016/S1352-2310(99)00515-4

Vancouver

Lohmann R, Lee RGM, Green NJL, Jones KC. Gas-particle partitioning of PCDD/Fs in daily air samples. Atmospheric Environment. 2000;34(16):2529-2537. doi: 10.1016/S1352-2310(99)00515-4

Author

Lohmann, Rainer ; Lee, Robert G. M. ; Green, Nicholas J. L. et al. / Gas-particle partitioning of PCDD/Fs in daily air samples. In: Atmospheric Environment. 2000 ; Vol. 34, No. 16. pp. 2529-2537.

Bibtex

@article{5dbfcbf12ad941f4ac3e9905d15c19e8,
title = "Gas-particle partitioning of PCDD/Fs in daily air samples.",
abstract = "Eight short-term (24–48 h) air samples were taken at Lancaster, UK, to study the gas–particle partitioning of PCDD/Fs. Sampling dates in autumn 1997 were selected with a view to minimising temperature fluctuation during the sampling events. ΣCl4-8DD/Fs (ΣTEQ) for the first 6 samples were 1.1–3.6 pg m−3 (15–44 fg TEQ m−3), typical of a rural site; two other samples had ΣCl4-8DD/Fs of 18 and 7.9 pg m−3, with 320 and 100 fg TEQ m−3. The observed gas–particle distributions varied from 0–34% particle-bound for Cl2/3DD/Fs to >70% for Cl6-8DD/Fs. Measured particle-bound fractions were compared to theoretical estimates of their distribution based on the Junge–Pankow model using three different reported sets of vapour pressures. The best correlation was obtained using vapour pressures derived from measured GC-retention time indices (Eitzer and Hites, 1988). Plotting log partition coefficient (Kp) versus log sub-cooled liquid vapour pressure (pL) gave excellent correlations with slopes of roughly −1 for all homologue groups. 2, 3, 7, 8-substituted congeners showed slopes of −1 for the first five sampling events. It is proposed that kinetic factors at the low ambient temperatures, coupled with additional emissions during the last sampling events resulted in non-equilibrium partitioning.",
keywords = "Gas-particle partitioning, Junge–Pankow, Dioxins, Furans, Vapour pressure",
author = "Rainer Lohmann and Lee, {Robert G. M.} and Green, {Nicholas J. L.} and Jones, {Kevin C.}",
year = "2000",
doi = "10.1016/S1352-2310(99)00515-4",
language = "English",
volume = "34",
pages = "2529--2537",
journal = "Atmospheric Environment",
issn = "1352-2310",
publisher = "PERGAMON-ELSEVIER SCIENCE LTD",
number = "16",

}

RIS

TY - JOUR

T1 - Gas-particle partitioning of PCDD/Fs in daily air samples.

AU - Lohmann, Rainer

AU - Lee, Robert G. M.

AU - Green, Nicholas J. L.

AU - Jones, Kevin C.

PY - 2000

Y1 - 2000

N2 - Eight short-term (24–48 h) air samples were taken at Lancaster, UK, to study the gas–particle partitioning of PCDD/Fs. Sampling dates in autumn 1997 were selected with a view to minimising temperature fluctuation during the sampling events. ΣCl4-8DD/Fs (ΣTEQ) for the first 6 samples were 1.1–3.6 pg m−3 (15–44 fg TEQ m−3), typical of a rural site; two other samples had ΣCl4-8DD/Fs of 18 and 7.9 pg m−3, with 320 and 100 fg TEQ m−3. The observed gas–particle distributions varied from 0–34% particle-bound for Cl2/3DD/Fs to >70% for Cl6-8DD/Fs. Measured particle-bound fractions were compared to theoretical estimates of their distribution based on the Junge–Pankow model using three different reported sets of vapour pressures. The best correlation was obtained using vapour pressures derived from measured GC-retention time indices (Eitzer and Hites, 1988). Plotting log partition coefficient (Kp) versus log sub-cooled liquid vapour pressure (pL) gave excellent correlations with slopes of roughly −1 for all homologue groups. 2, 3, 7, 8-substituted congeners showed slopes of −1 for the first five sampling events. It is proposed that kinetic factors at the low ambient temperatures, coupled with additional emissions during the last sampling events resulted in non-equilibrium partitioning.

AB - Eight short-term (24–48 h) air samples were taken at Lancaster, UK, to study the gas–particle partitioning of PCDD/Fs. Sampling dates in autumn 1997 were selected with a view to minimising temperature fluctuation during the sampling events. ΣCl4-8DD/Fs (ΣTEQ) for the first 6 samples were 1.1–3.6 pg m−3 (15–44 fg TEQ m−3), typical of a rural site; two other samples had ΣCl4-8DD/Fs of 18 and 7.9 pg m−3, with 320 and 100 fg TEQ m−3. The observed gas–particle distributions varied from 0–34% particle-bound for Cl2/3DD/Fs to >70% for Cl6-8DD/Fs. Measured particle-bound fractions were compared to theoretical estimates of their distribution based on the Junge–Pankow model using three different reported sets of vapour pressures. The best correlation was obtained using vapour pressures derived from measured GC-retention time indices (Eitzer and Hites, 1988). Plotting log partition coefficient (Kp) versus log sub-cooled liquid vapour pressure (pL) gave excellent correlations with slopes of roughly −1 for all homologue groups. 2, 3, 7, 8-substituted congeners showed slopes of −1 for the first five sampling events. It is proposed that kinetic factors at the low ambient temperatures, coupled with additional emissions during the last sampling events resulted in non-equilibrium partitioning.

KW - Gas-particle partitioning

KW - Junge–Pankow

KW - Dioxins

KW - Furans

KW - Vapour pressure

U2 - 10.1016/S1352-2310(99)00515-4

DO - 10.1016/S1352-2310(99)00515-4

M3 - Journal article

VL - 34

SP - 2529

EP - 2537

JO - Atmospheric Environment

JF - Atmospheric Environment

SN - 1352-2310

IS - 16

ER -