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Temperature dependence of the rain-gas and snow-gas partition coefficients for nearly a thousand chemicals.

Authors :
Yang PF
Ma WL
Xiao H
Hansen KM
Wang L
Sun JJ
Liu LY
Zhang ZF
Jia HL
Li YF
Source :
Chemosphere [Chemosphere] 2024 Aug; Vol. 362, pp. 142565. Date of Electronic Publication: 2024 Jun 11.
Publication Year :
2024

Abstract

Compared to the particle-gas partition coefficients (K <subscript>PG</subscript> ), the rain-gas (K <subscript>RG</subscript> ) and snow-gas (K <subscript>SG</subscript> ) partition coefficients are also essential in studying the environmental behavior and fate of chemicals in the atmosphere. While the temperature dependence for the K <subscript>PG</subscript> have been extensively studied, the study for K <subscript>RG</subscript> and K <subscript>SG</subscript> are still lacking. Adsorption coefficients between water surface-air (K <subscript>IA</subscript> ) and snow surface-air (K <subscript>JA</subscript> ), as well as partition coefficients between water-air (K <subscript>WA</subscript> ) and octanol-air (K <subscript>OA</subscript> ) are vital in calculating K <subscript>RG</subscript> and K <subscript>SG</subscript> . These four basic adsorption and partition coefficients are also temperature-dependent, given by the well-known two-parameters Antoine equation logK <subscript>XY</subscript>  = A <subscript>XY</subscript>  + B <subscript>XY</subscript> /T, where K <subscript>XY</subscript> is the adsorption or partition coefficients, A <subscript>XY</subscript> and B <subscript>XY</subscript> are Antoine parameters (XY stand for IA, JA, WA, and OA), and T is the temperature in Kelvin. In this study, the parameters A <subscript>XY</subscript> and B <subscript>XY</subscript> are calculated for 943 chemicals, and logK <subscript>XY</subscript> can be estimated at any ambient temperature for these chemicals using these Antoine parameters. The results are evaluated by comparing these data with published experimental and modeled data, and the results show reasonable accuracy. Based on these coefficients, temperature-dependence of logK <subscript>RG</subscript> and logK <subscript>SG</subscript> is studied. It is found that both logK <subscript>RG</subscript> and logK <subscript>SG</subscript> are linearly related to 1/T, and Antoine parameters for logK <subscript>RG</subscript> and logK <subscript>SG</subscript> are also estimated. Distributions of the 943 chemicals in the atmospheric phases (gas, particle, and rain/snow), are illustrated in a Chemical Space Map. The findings reveal that, at environmental temperatures and precipitation days, the dominant state for the majority of chemicals is the gaseous phase. All the A <subscript>XY</subscript> and B <subscript>XY</subscript> values for logK <subscript>SG</subscript> , logK <subscript>RG</subscript> , and basic adsorption and partition coefficients, both modeled by this study and collected from published work, are systematically organized into an accessible dataset for public utilization.<br />Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2024 Elsevier Ltd. All rights reserved.)

Details

Language :
English
ISSN :
1879-1298
Volume :
362
Database :
MEDLINE
Journal :
Chemosphere
Publication Type :
Academic Journal
Accession number :
38871187
Full Text :
https://doi.org/10.1016/j.chemosphere.2024.142565