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Theoretical study on the mechanisms, kinetics and risk assessment of OH radicals and Cl atom initiated transformation of HCFC-235fa in the atmosphere.

Authors :
Chi TX
Li XX
Ni S
Bai FY
Pan XM
Zhao Z
Source :
Physical chemistry chemical physics : PCCP [Phys Chem Chem Phys] 2024 Oct 02; Vol. 26 (38), pp. 24821-24832. Date of Electronic Publication: 2024 Oct 02.
Publication Year :
2024

Abstract

Hydrochlorofluorocarbons (HCFCs) are important greenhouse gases and ozone-depleting substances. Thus, a thorough understanding of their atmospheric fate is essential for preventing and controlling atmospheric pollution. Herein, the atmospheric transformation mechanism of CF <subscript>3</subscript> CH <subscript>2</subscript> CClF <subscript>2</subscript> (HCFC-235fa) by the OH radical and the Cl atom was carried out at the dual-level of CCSD(T)/aug-cc-pVTZ//M06-2X/6-311+G(d,p). The reaction rate coefficients were calculated using the multistructural canonical variational transition state theory with small curvature tunneling (MS-CVT/SCT) at 200-1000 K. The k <superscript>MS-CVT/SCT</superscript> (CF <subscript>3</subscript> CH <subscript>2</subscript> CClF <subscript>2</subscript> + OH) and k <superscript>MS-CVT/SCT</superscript> (CF <subscript>3</subscript> CH <subscript>2</subscript> CClF <subscript>2</subscript> + Cl) values are 9.05 × 10 <superscript>-15</superscript> and 1.95 × 10 <superscript>-17</superscript> cm <superscript>3</superscript> molecule <superscript>-1</superscript> s <superscript>-1</superscript> at 297 K, respectively. The results show that the role of OH is more important than Cl in the degradation of CF <subscript>3</subscript> CH <subscript>2</subscript> CClF <subscript>2</subscript> . The atmospheric lifetimes (83 days-77.93 years), ozone destruction potential (0.001-0.023), and global warming potentials (GWP <subscript>100</subscript> = 21.06-5157.35) of CF <subscript>3</subscript> CH <subscript>2</subscript> CClF <subscript>2</subscript> were assessed, and these results indicate that CF <subscript>3</subscript> CH <subscript>2</subscript> CClF <subscript>2</subscript> is atmospherically persistent and environmentally unfriendly. The evolution mechanisms of CF <subscript>3</subscript> C·HCClF <subscript>2</subscript> , CF <subscript>3</subscript> C(OO˙)HCClF <subscript>2</subscript> , and CF <subscript>3</subscript> C(O˙)HCClF <subscript>2</subscript> in the presence of O <subscript>2</subscript> , HO <subscript>2</subscript> ˙, and NO were investigated and discussed. The resulting products of CF <subscript>3</subscript> CH <subscript>2</subscript> CClF <subscript>2</subscript> are mostly highly oxidized multi-functional compounds in the forms of aldehydes, ketones, and organic nitrates. A computational assessment of acute and chronic toxicities was performed at three levels of nutrition in order to improve the understanding of the potential toxicity of CF <subscript>3</subscript> CH <subscript>2</subscript> CClF <subscript>2</subscript> and its degradation products to the aquatic environment. The acidification potential of CF <subscript>3</subscript> CH <subscript>2</subscript> CClF <subscript>2</subscript> was calculated to be 1.141 and presumed to contribute to the formation of acid rain. The results may contribute to describing HCFCs' atmospheric fate, persistence, and environmental risks.

Details

Language :
English
ISSN :
1463-9084
Volume :
26
Issue :
38
Database :
MEDLINE
Journal :
Physical chemistry chemical physics : PCCP
Publication Type :
Academic Journal
Accession number :
39290189
Full Text :
https://doi.org/10.1039/d4cp02323d