Theoretical study on the mechanisms, kinetics and risk assessment of OH radicals and Cl atom initiated transformation of HCFC-235fa in the atmosphere.
Tai-Xing ChiXin-Xin LiShuang NiFeng-Yang BaiXiu-Mei PanZhen ZhaoPublished in: Physical chemistry chemical physics : PCCP (2024)
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 3 CH 2 CClF 2 (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 MS-CVT/SCT (CF 3 CH 2 CClF 2 + OH) and k MS-CVT/SCT (CF 3 CH 2 CClF 2 + Cl) values are 9.05 × 10 -15 and 1.95 × 10 -17 cm 3 molecule -1 s -1 at 297 K, respectively. The results show that the role of OH is more important than Cl in the degradation of CF 3 CH 2 CClF 2 . The atmospheric lifetimes (83 days-77.93 years), ozone destruction potential (0.001-0.023), and global warming potentials (GWP 100 = 21.06-5157.35) of CF 3 CH 2 CClF 2 were assessed, and these results indicate that CF 3 CH 2 CClF 2 is atmospherically persistent and environmentally unfriendly. The evolution mechanisms of CF 3 C·HCClF 2 , CF 3 C(OO˙)HCClF 2 , and CF 3 C(O˙)HCClF 2 in the presence of O 2 , HO 2 ˙, and NO were investigated and discussed. The resulting products of CF 3 CH 2 CClF 2 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 3 CH 2 CClF 2 and its degradation products to the aquatic environment. The acidification potential of CF 3 CH 2 CClF 2 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.
Keyphrases
- cystic fibrosis
- risk assessment
- room temperature
- particulate matter
- human health
- mass spectrometry
- multiple sclerosis
- physical activity
- hepatitis b virus
- molecular dynamics
- nitric oxide
- liver failure
- signaling pathway
- intensive care unit
- cell proliferation
- pi k akt
- acute respiratory distress syndrome
- atomic force microscopy