首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >OH reaction rate constant, IR absorption spectrum, ozone depletion potentials and global warming potentials of 2-bromo-3,3,3-trifluoropropene
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OH reaction rate constant, IR absorption spectrum, ozone depletion potentials and global warming potentials of 2-bromo-3,3,3-trifluoropropene

机译:2-溴-3,3,3-三氟丙烯的OH反应速率常数,IR吸收光谱,臭氧消耗势和全球变暖势

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The rate constant for the gas phase reaction of OH radicals with BTP (2-bromo-3,3,3-trifluoropropene, CH_2 = CBrCF_3) was measured using a flash photolysis resonance-fluorescence technique over the temperature range 220 K to 370 K. The Arrhenius plot was found to exhibit noticeable curvature. The temperature dependence of the rate constant can be represented as k_(BTP)(220 - 370 K) = 4.85 × 10~(-13) × (T/298)~(0.92) × exp{+613/T} cm~3 molecule~(-1) s~(-1). For atmospheric modeling purposes, k_(BTP)(T) can be equally well represented by the standard Arrhenius expression k_(BTP)(220 - 298 K) = 1.05 × 10~(-12) × exp{+381/T} cm~3 molecule~(-1) s~(-1). The IR absorption cross-sections of BTP were also measured between 450 cm~(-1) and 1900 cm~(-1). BTP atmospheric lifetime, Ozone Depletion Potential (ODP), and Global Warming Potential (GWP) were evaluated in the Whole Atmosphere Community Climate Model for land emissions from 30 to 60°N and from 60°S to 60°N. The global, annual average atmospheric lifetime of BTP in the former scenario was 7.0 days, its ODP was 0.0028, and its GWP (100-yr time horizon) was 0.0050; in the latter scenario, the global, annual average BTP lifetime was 4.3 days, ODP was 0.0052, and 100-yr GWP was 0.0028. The short lifetime, low ODP, and low GWP indicate that BTP should have minimal effects on ozone and climate. Little BTP reaches the stratosphere in either emission scenario, but 27% of the ozone loss in the 30 to 60°N scenario and 46% of the ozone loss in the 0°S to 60°N scenario occurs above the tropopause due to Br_y from BTP.
机译:使用快速光解共振荧光技术在220 K至370 K的温度范围内测量OH自由基与BTP(2-溴-3,3,3-三氟丙烯,CH_2 = CBrCF_3)的气相反应速率常数。发现阿累尼乌斯图显示出明显的曲率。速率常数的温度依赖性可以表示为k_(BTP)(220 - 370 K)= 4.85×10〜(-13)×(T / 298)〜(0.92)×exp {+ 613 / T} cm〜 3分子〜(-1)s〜(-1)。出于大气建模的目的,k_(BTP)(T)可以用标准阿伦尼乌斯表达式k_(BTP)(220 - 298 K)= 1.05×10〜(-12)×exp {+ 381 / T} cm表示。 〜3分子〜(-1)s〜(-1)。还测量了BTP的IR吸收截面在450cm-1(-1)至1900cm-1(-1)之间。 BTP大气寿命,臭氧消耗潜能(ODP)和全球变暖潜能(GWP)在“整个大气社区气候模型”中评估了30至60°N和60°S至60°N的土地排放。在前一种情况下,BTP的全球年平均大气寿命为7.0天,ODP为0.0028,GWP(100年时间范围)为0.0050;在后一种情况下,全球年均BTP寿命为4.3天,ODP为0.0052,100年GWP为0.0028。寿命短,ODP低和GWP低表明BTP对臭氧和气候的影响应最小。在任一排放情景中,很少有BTP到达平流层,但是在30至60°N情景中,臭氧损失的27%和在0°S至60°N情景中臭氧损失的46%发生在对流层顶,这是由于BTP。

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