Laboratoire de Spectrométrie Physique, Université Joseph Fourier, 38402 St. Martin d'Hères, France.
J Phys Chem A. 2010 Sep 16;114(36):9855-63. doi: 10.1021/jp103266m.
The absorption cross sections of 18 isotopologues of the ozone molecule have been calculated in the range of the Hartley-Huggins bands (27000-55000 cm(-1)). All 18 possible ozone isotopologues made with (16)O, (17)O, and (18)O have been considered, with emphasis on those of geophysics interest like (16)O(3) (17)O(16)O(2), (16)O(17)O(16)O, (18)O(16)O(2), and (16)O(18)O(16)O. We have used the MCTDH algorithm to propagate wavepackets. As an initial wavepacket, we took the vibrational ground state multiplied by the transition dipole moment surface. The cross sections have been obtained from the autocorrelation function of this wavepacket. Only two potential energy surfaces (PESs) and the corresponding transition dipole moment are involved in the calculation. The dissociating R state has been omitted. The calculations have been performed only for J = 0. The comparison with the experimental absorption cross sections of (16)O(3) and (18)O(3) has been performed after an empirical smoothing which mimics the rotational envelop. The isotopologue dependence of the cross sections of 18 isotopologues can be split into two energy ranges, (a) from 27000 to 32000 cm(-1), the Huggins band, which is highly structured, and (b) from 32000 to 55000 cm(-1), the main part of the cross section which has a bell shape, the Hartley band. This bell-shaped envelop has been characterized by a new analytic model depending on only four parameters, amplitude, center, width, and asymmetry. The isotopologue dependence of these parameters reveals the tiny differences between the absorption cross sections of the various isotopologues. In contrast to the smooth shape of the Hartley band, the Huggins band exhibits pronounced vibrational structures and therefore shows large isotopologue differences which may induce a significant isotopologue dependence of the ozone photodissociation rates under actinic flux.
在哈特利-哈金斯带(27000-55000 cm(-1))范围内,计算了 18 种臭氧分子的同位素分子的吸收截面。所有可能的 18 种由 (16)O、(17)O 和 (18)O 制成的臭氧同位素都被考虑在内,重点是那些具有地球物理意义的同位素,如 (16)O(3) (17)O(16)O(2)、(16)O(17)O(16)O、(18)O(16)O(2)和 (16)O(18)O(16)O。我们使用 MCTDH 算法来传播波包。作为初始波包,我们采用了乘以跃迁偶极矩表面的振动基态。截面是从这个波包的自相关函数中得到的。计算中只涉及两个势能面(PES)和相应的跃迁偶极矩。解离的 R 态被忽略了。仅对 J = 0 进行了计算。在进行经验平滑处理后,与 (16)O(3)和 (18)O(3)的实验吸收截面进行了比较,该平滑处理模拟了旋转包络。18 种同位素的截面的同位素依赖性可以分为两个能量范围:(a) 从 27000 到 32000 cm(-1),即哈金斯带,它具有高度结构化;(b) 从 32000 到 55000 cm(-1),即截面的主要部分,呈钟形,即哈特利带。这种钟形包络由一个仅依赖于四个参数的新解析模型来描述,即幅度、中心、宽度和不对称性。这些参数的同位素依赖性揭示了各种同位素的吸收截面之间的微小差异。与哈特利带的平滑形状相比,哈金斯带表现出明显的振动结构,因此表现出较大的同位素差异,这可能会导致光解率在光强通量下具有显著的同位素依赖性。