首页> 外文OA文献 >UV and infrared absorption spectra, atmospheric lifetimes, and ozone depletion and global warming potentials for CCl2FCCl2F (CFC-112), CCl3CClF2 (CFC-112a), CCl3CF3 (CFC-113a), and CCl2FCF3 (CFC-114a)
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UV and infrared absorption spectra, atmospheric lifetimes, and ozone depletion and global warming potentials for CCl2FCCl2F (CFC-112), CCl3CClF2 (CFC-112a), CCl3CF3 (CFC-113a), and CCl2FCF3 (CFC-114a)

机译:CCl2FCCl2F(CFC-112),CCl3CClF2(CFC-112a),CCl3CF3(CFC-113a)和CCl2FCF3(CFC-114a)的紫外线和红外吸收光谱,大气寿命以及臭氧消耗和全球变暖潜能

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摘要

The potential impact of CCl2FCF3 (CFC-114a) and the recently observed CCl2FCCl2F (CFC-112), CCl3CClF2 (CFC-112a), and CCl3CF3 (CFC-113a) chlorofluorocarbons (CFCs) on stratospheric ozone and climate is presently not well characterized. In this study, the UV absorption spectra of these CFCs were measured between 192.5 and 235 nm over the temperature range 207–323 K.Precise parameterizations of the UV absorption spectra are presented. A 2-D atmospheric model was used to evaluate the CFC atmospheric loss processes, lifetimes, ozone depletion potentials (ODPs), and the associated uncertainty ranges in these metrics due to the kinetic and photochemical uncertainty.The CFCs are primarily removed in the stratosphere by short-wavelength UV photolysis with calculated global annually averaged steady-state lifetimes (years) of 63.6 (61.9–64.7), 51.5 (50.0–52.6), 55.4 (54.3–56.3), and 105.3 (102.9–107.4) for CFC-112, CFC-112a, CFC-113a, and CFC-114a, respectively. The range of lifetimes given in parentheses is due to the 2σ uncertainty in the UV absorption spectra and O(1D) rate coefficients included in the model calculations. The 2-D model was also used to calculate the CFC ozone depletion potentials (ODPs) with values of 0.98, 0.86, 0.73, and 0.72 obtained for CFC-112, CFC-112a, CFC-113a, and CFC-114a, respectively. Using the infraredabsorption spectra and lifetimes determined in this work, the CFC global warming potentials (GWPs) were estimated to be 4260 (CFC-112), 3330 (CFC-112a), 3650 (CFC-113a), and 6510 (CFC-114a) for the 100-year time horizon.
机译:CCl2FCF3(CFC-114a)和最近观察到的CCl2FCCl2F(CFC-112),CCl3CClF2(CFC-112a)和CCl3CF3(CFC-113a)氯氟烃(CFC)对平流层臭氧和气候的潜在影响目前尚不十分清楚。在这项研究中,在207–323 K的温度范围内,测量了这些CFC的UV吸收光谱,范围为192.5至235 nm。给出了UV吸收光谱的精确参数化。由于动力学和光化学不确定性,使用2-D大气模型评估CFC大气损失过程,寿命,臭氧消耗潜能(ODP)以及这些度量标准中的相关不确定性范围。 CFC-112的短波紫外线光解,其全球年平均稳态寿命(年)计算为63.6(61.9-64.7),51.5(50.0-52.6),55.4(54.3-56.3)和105.3(102.9-107.4) ,CFC-112a,CFC-113a和CFC-114a。括号中给出的寿命范围是由于模型计算中包括的UV吸收光谱中2σ不确定性和O(1D)速率系数引起的。 2-D模型还用于计算CFC-112,CFC-112a,CFC-113a和CFC-114a分别获得的0.98、0.86、0.73和0.72值的CFC臭氧消耗潜能(ODP)。使用这项工作中确定的红外吸收光谱和寿命,CFC全球变暖潜势(GWP)估计为4260(CFC-112),3330(CFC-112a),3650(CFC-113a)和6510(CFC-114a) )的100年时间范围。

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