Chemical Investigation on the Mechanism and Kinetics of the Atmospheric Degradation Reaction of Trichlorofluoroethene by OH• and Its Subsequent Fate in the Presence of O2/NOx

被引:0
|
作者
Shiroudi, Abolfazl [1 ,2 ]
Czub, Jacek [1 ,2 ]
Altarawneh, Mohammednoor [3 ]
机构
[1] Gdansk Univ Technol, Dept Phys Chem, Narutowicza 11-12, PL-80233 Gdansk, Poland
[2] Gdansk Univ Technol, BioTechMed Ctr, PL-80233 Gdansk, Poland
[3] United Arab Emirates Univ, Dept Chem & Petr Engn, Sheikh Khalifa bin Zayed St, Al Ain 15551, U Arab Emirates
关键词
atmospheric lifetime; global warming potentials; rate coefficient; POCP; trichlorofluoroethene; OZONE CREATION POTENTIALS; ORGANIC-COMPOUNDS; THERMOCHEMICAL KINETICS; DEPLETION POTENTIALS; DENSITY FUNCTIONALS; TROPOSPHERE PRODUCT; GAS-PHASE; CHEMISTRY; OXIDATION; RADICALS;
D O I
10.1002/cphc.202300665
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The M06-2X/6-311++G(d,p) level of theory was used to examine the degradation of Trichlorofluoroethene (TCFE) initiated by OH center dot radicals. Additionally, the coupled-cluster single-double with triple perturbative [CCSD(T)] method was employed to refine the single-point energies using the complete basis set extrapolation approach. The results indicated that OH-addition is the dominant pathway. OH center dot adds to both the C1 and C2 carbons, resulting in the formation of the C(OH)Cl-2-(CClF)-C-center dot and (CCl2)-C-center dot-C(OH)ClF species. The associated barrier heights were determined to be 1.11 and -0.99 kcal mol(-1), respectively. Furthermore, the energetic and thermodynamic parameters show that pathway 1 exhibits greater exothermicity and exergonicity compared to pathway 2, with differences of 8.11 and 8.21 kcal mol(-1), correspondingly. The primary pathway involves OH addition to the C2 position, with a rate constant of 6.2x10(-13) cm(3) molecule(-1) sec(-1) at 298 K. This analysis served to estimate the atmospheric lifetime, along with the photochemical ozone creation potential (POCP) and ozone depletion potential (ODP). It yielded an atmospheric lifetime of 8.49 days, an ODP of 4.8x10(-4), and a POCP value of 2.99, respectively. Radiative forcing efficiencies were also estimated at the M06-2X/6-311++G(d,p) level. Global warming potentials (GWPs) were calculated for 20, 100, and 500 years, resulting in values of 9.61, 2.61, and 0.74, respectively. TCFE is not expected to make a significant contribution to the radiative forcing of climate change. The results obtained from the time-dependent density functional theory (TDDFT) indicated that TCFE and its energized adducts are unable to photolysis under sunlight in the UV and visible spectrum. Secondary reactions involve the [TCFE-OH-O-2](center dot) peroxy radical, leading subsequently to the [TCFE-OH-O](center dot) alkoxy radical. It was found that the alkoxy radical resulting from the peroxy radical can lead to the formation of phosgene (COCl2) and carbonyl chloride fluoride (CClFO), with phosgene being the primary product.
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页数:17
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