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三氯氟乙烯与OH⋅的大气降解反应机理及动力学的化学研究及其在O /NOx存在下的后续归宿

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

作者信息

Shiroudi Abolfazl, Czub Jacek, Altarawneh Mohammednoor

机构信息

Department of Physical Chemistry, Gdańsk University of Technology, Narutowicza 11/12, Gdańsk, 80-233, Poland.

BioTechMed Center, Gdańsk University of Technology, Gdańsk, 80-233, Poland.

出版信息

Chemphyschem. 2024 Feb 1;25(3):e202300665. doi: 10.1002/cphc.202300665. Epub 2023 Dec 4.

Abstract

The M06-2X/6-311++G(d,p) level of theory was used to examine the degradation of Trichlorofluoroethene (TCFE) initiated by OH⋅ 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⋅ adds to both the C1 and C2 carbons, resulting in the formation of the C(OH)Cl -⋅CClF and ⋅CCl -C(OH)ClF species. The associated barrier heights were determined to be 1.11 and -0.99 kcal mol , 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 , correspondingly. The primary pathway involves OH addition to the C2 position, with a rate constant of 6.2×10  cm molecule sec 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 4.8×10 , 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 ]⋅ peroxy radical, leading subsequently to the [TCFE-OH-O]⋅ alkoxy radical. It was found that the alkoxy radical resulting from the peroxy radical can lead to the formation of phosgene (COCl ) and carbonyl chloride fluoride (CClFO), with phosgene being the primary product.

摘要

采用M06 - 2X/6 - 311++G(d,p)理论水平研究了OH⋅自由基引发的三氯氟乙烯(TCFE)降解过程。此外,采用耦合簇单双激发并包含三重微扰的[CCSD(T)]方法,利用完全基组外推法对单点能量进行了优化。结果表明,OH加成是主要途径。OH⋅加成到C1和C2碳上,分别形成C(OH)Cl -⋅CClF和⋅CCl -C(OH)ClF物种。其相关势垒高度分别确定为1.11和 -0.99 kcal mol 。此外,能量和热力学参数表明,与途径2相比,途径1表现出更大的放热性和放能性,相应的差值分别为8.11和8.21 kcal mol 。主要途径是OH加成到C2位,在298 K时的速率常数为6.2×10  cm molecule sec 。该分析用于估算大气寿命以及光化学臭氧生成潜力(POCP)和臭氧消耗潜力(ODP)。结果分别得到大气寿命为8.49天,ODP为4.8×10 ,POCP值为2.99。还在M06 - 2X/6 - 311++G(d,p)水平上估算了辐射强迫效率。计算了20年、100年和500年的全球变暖潜能值(GWP),结果分别为9.61、2.61和0.74。预计TCFE对气候变化的辐射强迫不会有显著贡献。时变密度泛函理论(TDDFT)的结果表明,TCFE及其激发加合物在紫外和可见光谱的太阳光下无法发生光解。二级反应涉及[TCFE - OH - O ]⋅过氧自由基,随后生成[TCFE - OH - O]⋅烷氧自由基。发现过氧自由基产生的烷氧自由基可导致光气(COCl )和碳酰氯氟化物(CClFO)的形成,其中光气是主要产物。

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