期刊
CHEMOSPHERE
卷 273, 期 -, 页码 -出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.chemosphere.2020.128865
关键词
SVOCs; Gas/particle partitioning; Slopes; Equilibrium; Steady state; Polar regions
资金
- National Natural Science Foundation of China [21577030]
- State Key Laboratory of Urban Water Resource and Environment (Harbin Institute of Technology) [2019DX04]
- Polar Academy, Harbin Institute of Technology [PA-HIT-201901]
- Heilongjiang Provincial Key laboratory of Polar Environment and Ecosystem (HPKL-PEE), HIT
Gas/particle partitioning plays a key role in the transport and fate of semi-volatile organic compounds in the atmosphere, with the equilibrium assumption being challenged by experimental findings. Analytical equations were developed to calculate parameters related to partitioning, revealing that deviations from theoretical predictions cannot be solely explained by experimental or statistical artifacts.
Gas/particle partitioning governs the transport and fate of semi-volatile organic compounds (SVOCs) released to the atmosphere. The partition quotient of SVOCs, K-P, is related to their subcooled liquid vapor pressure (logK(P) = m(p) logP(L) + b(p)) and to their octanol-air partition coefficient (logK(P) = m(o) logK(OA) + b(o)). Previous theory predicts that -m(p) and m(o) should be close to, or equal to 1 based on the assumption that gas- and particle-phases are at equilibrium in the atmosphere. Here, we develop analytical equations to calculate m(o) and b(o) as functions of logK(OA) and m(p) and b(p) as functions of logP(L). We find that experimental, analytical, or statistical artifacts and other reported factors are not the leading causes for deviations of the slopes, m(p) and m(o), from -1 and 1, respectively. Rather, it is the inherent parameter, K-OA, that determines m(o) and b(o), and equivalently, P-L is the major parameter determining m(p) and b(p), and such deviations are evidence that equilibrium is an inappropriate assumption. In contrast, the actual steady-state between gas and particle phases of SVOCs leads that their -m(p) and m(o) should range from 0 to 1, implying that equilibrium is a reasonable assumption only when -m(p) and m(o) are larger than 0.49. To illustrate these points, we provide a detailed discussion of the global atmospheric transport of polybrominated diphenyl ethers (PBDEs) with emphasis on Polar Regions where low air temperatures favor a special steady-state, where their slopes m(p) and m(o) can reach 0, indicating a constant value of logK(P) (-1.53). (C) 2020 Elsevier Ltd. All rights reserved.
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