Earth System Research Laboratory, Chemical Sciences Division, National Oceanic and Atmospheric Administration, 325 Broadway, Boulder, Colorado 80305-3328, USA.
J Phys Chem A. 2010 Apr 8;114(13):4619-33. doi: 10.1021/jp100527z.
Rate coefficients, k, for the gas-phase reaction of the OH radical with CH(2)=CHF (k(1)) and CH(2)=CF(2) (k(2)) were measured under pseudo-first-order conditions in OH using pulsed laser photolysis to produce OH and laser-induced fluorescence (PLP-LIF) to detect it. Rate coefficients were measured over a range of temperature (220-373 K) and bath gas pressure (20-600 Torr; He, N(2)). The rate coefficients were found to be independent of pressure. The measured rate coefficient for reaction 1 at room temperature was k(1)(296 K) = (5.18 +/- 0.50) x 10(-12) cm(3) molecule(-1) s(-1), independent of pressure, and the temperature dependence is given by the Arrhenius expression k(1)(T) = (1.75 +/- 0.20) x 10(-12) exp[(316 +/- 25)/T] cm(3) molecule(-1) s(-1); the rate coefficients for reaction 2 were k(2)(296 K) = (2.79 +/- 0.25) x 10(-12) cm(3) molecule(-1) s(-1) and k(2)(T) = (1.75 +/- 0.20) x 10(-12) exp[(140 +/- 20)/T] cm(3) molecule(-1) s(-1). The quoted uncertainties are 2sigma (95% confidence level) and include estimated systematic errors. The fall-off parameters for reaction 2 of k(infinity) = 3 x 10(-12) cm(3) molecule(-1) s(-1) and k(0)(296 K) = 1.8 x 10(-28) cm(6) molecule(-2) s(-1) with F(c) = 0.6 reproduce the room temperature data obtained in this study combined with the low pressure rate coefficient data from Howard (J. Chem. Phys. 1976, 65, 4771). OH radical formation was observed for reactions 1 and 2 in the presence of O(2), and the mechanism was investigated using (18)OH and OD rate coefficient measurements with CH(2)=CHF and CH(2)=CF(2) over a range of temperature (260-373 K) and pressure (20-100 Torr, He). Quantum chemical calculations using density functional theory (DFT) were used to determine the geometries and energies of the reactants and adducts formed in reactions 1 and 2 and the peroxy radicals formed following the addition of O(2). The atmospheric lifetimes of CH(2)=CHF and CH(2)=CF(2) due to loss by reaction with OH are approximately 2 and 4 days, respectively. Infrared absorption spectra of CH(2)=CHF and CH(2)=CF(2) were measured, and global warming potentials (GWP) values of 0.7 for CH(2)=CHF and 0.9 for CH(2)=CF(2) were obtained for the 100 year time horizon.
速率系数 k,用于测量 OH 自由基与 CH(2)=CHF(k(1))和 CH(2)=CF(2)(k(2))的气相反应,在 OH 中使用脉冲激光光解产生 OH 和激光诱导荧光 (PLP-LIF)来检测它。在 220-373 K 的温度范围内和 20-600 Torr 的浴气压(He、N(2))下测量了速率系数。发现速率系数与压力无关。在室温下反应 1 的测量速率系数为 k(1)(296 K)=(5.18+/-0.50)x10(-12)cm(3)molecule(-1)s(-1),与压力无关,温度依赖性由阿仑尼乌斯表达式给出 k(1)(T)=(1.75+/-0.20)x10(-12)exp[(316+/-25)/T]cm(3)molecule(-1)s(-1);反应 2 的速率系数为 k(2)(296 K)=(2.79+/-0.25)x10(-12)cm(3)molecule(-1)s(-1)和 k(2)(T)=(1.75+/-0.20)x10(-12)exp[(140+/-20)/T]cm(3)molecule(-1)s(-1)。给出的不确定度为 2sigma(95%置信水平),包括估计的系统误差。反应 2 的崩溃参数 k(infinity)=(3)x10(-12)cm(3)molecule(-1)s(-1)和 k(0)(296 K)=(1.8)x10(-28)cm(6)molecule(-2)s(-1),F(c)=(0.6),可重现本研究中获得的室温数据以及 Howard 的低压速率系数数据(J.Chem.Phys.1976,65,4771)。在存在 O(2)的情况下,观察到反应 1 和 2 中形成了 OH 自由基,并且使用(18)OH 和 OD 速率系数测量与 CH(2)=CHF 和 CH(2)=CF(2),在 260-373 K 的温度范围和 20-100 Torr(He)的压力下,研究了其反应机制。使用密度泛函理论(DFT)的量子化学计算用于确定反应 1 和 2 中形成的反应物和加合物以及在添加 O(2)后形成的过氧基的几何形状和能量。由于与 OH 反应而导致 CH(2)=CHF 和 CH(2)=CF(2)损失的大气寿命分别约为 2 和 4 天。测量了 CH(2)=CHF 和 CH(2)=CF(2)的红外吸收光谱,并获得了 100 年时间跨度下 CH(2)=CHF 的全球升温潜能值(GWP)为 0.7 和 CH(2)=CF(2)的 GWP 值为 0.9。