Ojekull J, Andersson P U, Pettersson J B C, Marković N, Thomas R D, Al Khalili A, Ehlerding A, Osterdahl F, af Ugglas M, Larsson M, Danared H, Källberg A
Department of Chemistry, Atmospheric Science, Göteborg University, SE-412 96 Göteborg, Sweden.
J Chem Phys. 2008 Jan 28;128(4):044311. doi: 10.1063/1.2823062.
Dissociative recombination (DR) of water cluster ions H(+)(H(2)O)(n) (n=4-6) with free electrons has been studied at the heavy-ion storage ring CRYRING (Manne Siegbahn Laboratory, Stockholm University). For the first time, branching ratios have been determined for the dominating product channels and absolute DR cross sections have been measured in the energy range from 0.001 to 0.7 eV. Dissociative recombination is concluded to result in extensive fragmentation for all three cluster ions, and a maximum number of heavy oxygen-containing fragments is produced with a probability close to unity. The branching ratio results agree with earlier DR studies of smaller water cluster ions where the channel nH(2)O+H has been observed to dominate and where energy transfer to internal degrees of freedom has been concluded to be highly efficient. The absolute DR cross sections for H(+)(H(2)O)(n) (n=4-6) decrease monotonically with increasing energy with an energy dependence close to E(-1) in the lower part of the energy range and a faster falloff at higher energies, in agreement with the behavior of other studied heavy ions. The cross section data have been used to calculate DR rate coefficients in the temperature range of 10-2000 K. The results from storage ring experiments with water cluster ions are concluded to partly confirm the earlier results from afterglow experiments. The DR rate coefficients for H(+)(H(2)O)(n) (n=1-6) are in general somewhat lower than reported from afterglow experiments. The rate coefficient tends to increase with increasing cluster size, but not in the monotonic way that has been reported from afterglow experiments. The needs for further experimental studies and for theoretical models that can be used to predict the DR rate of polyatomic ions are discussed.
在位于斯德哥尔摩大学曼内·西格巴恩实验室的重离子储存环CRYRING上,研究了水团簇离子H⁺(H₂O)ₙ(n = 4 - 6)与自由电子的离解复合反应。首次测定了主要产物通道的分支比,并在0.001至0.7 eV的能量范围内测量了绝对离解复合截面。研究得出结论,离解复合会导致所有这三种团簇离子发生广泛的碎片化,并且产生大量含重氧碎片的概率接近于1。分支比结果与早期对较小水团簇离子的离解复合研究一致,在早期研究中观察到通道nH₂O + H占主导,并且得出结论认为,向内部自由度的能量转移非常高效。H⁺(H₂O)ₙ(n = 4 - 6)的绝对离解复合截面随能量增加单调下降,在能量范围较低部分的能量依赖性接近E⁻¹,在较高能量下下降更快,这与其他研究的重离子的行为一致。利用这些截面数据计算了10 - 2000 K温度范围内的离解复合速率系数。得出结论,水团簇离子储存环实验的结果部分证实了早期余辉实验结果。H⁺(H₂O)ₙ(n = 1 - 6)的离解复合速率系数总体上略低于余辉实验报道的值。该速率系数倾向于随团簇尺寸增大而增加,但并非如余辉实验报道的那样呈单调增加。讨论了进一步开展实验研究以及建立可用于预测多原子离子离解复合速率的理论模型的必要性。