人为气体 CHF2OCH2CF2CHF2 (HFE-356pcf3) 的反应:气候影响和羰基中间体的形成

Makroni Lily, Shemphang Hynniewta, Xiaofan Lv, Lingyan Wu*, Stanley Numbonui Tasheh, Julius Numbonui Ghogomu, Asit K. Chandra*, Narcisse Tsona Tchinda* and Lin Du*, 
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引用次数: 0

摘要

本研究对 CHF2OCH2CF2CHF2 + OH 反应及其对大气的影响进行了详细的理论研究。已确定 CHF2OCH2CF2CHF2 的 12 种构象,本研究考虑了低于 4.184 kJ mol-1 的三种最低能量构象。速率系数的计算采用了基于 DFT 的 M06-2X/6-311++g(d,p) 方法,并结合了典型转变态理论(CTST)和可变反应坐标-可变转变态理论(VRC-VTST)。在 298 K 时,我们计算出的速率系数为 2.96 × 10-14 cm3 molecule-1 s-1,与实验结果非常接近。这项工作研究了 CHF2OCH2CF2CHF2 的臭氧形成潜力(OFP)和大气降解途径。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Reactions of Anthropogenic Gas CHF2OCH2CF2CHF2 (HFE-356pcf3): Climatic Influences and Formation of Carbonyl Intermediates

Reactions of Anthropogenic Gas CHF2OCH2CF2CHF2 (HFE-356pcf3): Climatic Influences and Formation of Carbonyl Intermediates

This work presents a detailed theoretical study of the CHF2OCH2CF2CHF2 + OH reaction and its atmospheric implications. Twelve conformers of CHF2OCH2CF2CHF2 have been identified, and the three lowest energy conformers below 4.184 kJ mol–1 were considered in this work. The rate coefficient is calculated using the DFT-based M06-2X/6-311++g(d,p) method combined with canonical transition state theory (CTST) and variable reaction coordinates–variational transition state theory (VRC-VTST). At 298 K, our calculated rate coefficient of 2.96 × 10–14 cm3 molecule–1 s–1 is very close to the experimental result. This work investigates the ozone formation potential (OFP) and atmospheric degradation pathways of CHF2OCH2CF2CHF2.

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