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Vector properties of the O(D-1(2)) fragment produced from the photolysis of ozone in the wavelength range of 298 to 320 nm

机译:臭氧光解在298至320 nm波长范围内产生的O(D-1(2))片段的矢量性质

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The speed averaged translational anisotropy and electronic angular momentum polarization of the O(D-1(2)) atomic fragment formed from the photodissociation of ozone in the atmospherically important long wavelength region of the Hartley band (298 to 320 nm) have been measured using resonance enhanced multiphoton ionization time of flight mass spectrometry. The translational anisotropy parameter, beta, is found to decline from 1.1 for photolysis at 300 nm to a minimum value of 0 at 310 nm which is the threshold for production of O(D-1(2)) in conjunction with the O-2(a (1)Delta(g)v=0) molecular cofragment. For photolysis wavelengths greater than 310 nm, O(D-1(2)) is formed from the dissociation of internally excited ozone molecules. The corresponding beta parameters are markedly lower than for atomic fragments produced with the same speed from the photolysis of ground state ozone molecules. This result is consistent with two different pathways contributing to the photolysis of internally excited ozone at the longest wavelengths studied corresponding to initial internal excitation either in the symmetric or asymmetric stretching vibration. In addition, the polarization of the atomic angular momentum has been determined with the incoherent polarization parameters a(0)(2)(parallel to) and a(0)(2)(perpendicular to) increasing from values of -0.53 and -0.62 at 300 nm to -0.37 and -0.19 at 317 nm, consistent with the increasing contribution from the photolysis of internally excited ozone as the dissociation wavelength lengthens. Evaluation of these alignment parameters allows the populations of the magnetic substrates, m(j), to be determined. For example, for a photolysis wavelength of 303 nm the populations of m(j)=0,+/- 1,+/- 2 are in the ratio of 0.36: 0.56: 0.08 and this ratio is essentially independent of the photolysis wavelength. The coherent contribution to the atomic polarization is quantified by the Re{a(1)(2)(parallel to,perpendicular to)} and Im{a(1)(1)(parallel to,perpendicular to)} parameters and these are found to vary from -0.21 and 0.21 at 300 nm to -0.04 and 0.24 at 313 nm, respectively. (c) 2006 American Institute of Physics.
机译:已使用以下方法测量了O(D-1(2))原子碎片的速度平均平移各向异性和电子角动量极化,该碎片是由臭氧在哈特利谱带的重要大气长波长区域(298至320 nm)中进行光解而形成的共振增强多光子电离飞行时间质谱。发现平移各向异性参数β从300 nm处的光解作用的1.1降低到310 nm处的最小值0,这是与O-2结合产生O(D-1(2))的阈值(a(1)Delta(g)v = 0)分子共碎片。对于大于310 nm的光解波长,由内部激发的臭氧分子的解离形成O(D-1(2))。相应的β参数显着低于基态臭氧分子光解以相同速度产生的原子碎片的参数。该结果与两个不同的路径一致,这两个路径有助于内部激发的臭氧在研究的最长波长处的光解,这对应于对称或不对称拉伸振动中的初始内部激发。另外,原子相角动量的极化是由非相干极化参数a(0)(2)(平行于)和a(0)(2)(垂直于)确定的,从-0.53和-0.62的值增加随着解离波长的延长,内部激发的臭氧的光解作用的增加,与300 nm处的-0.37和317 nm处的-0.19一致。对这些对准参数的评估允许确定磁性衬底的总体m(j)。例如,对于303nm的光解波长,m(j)= 0,+ /-1,+ /-2的群体的比率为0.36∶0.56∶0.08,并且该比率基本上与光解波长无关。对原子极化的相干贡献由Re {a(1)(2)(平行于,垂直于)}和Im {a(1)(1)(平行于,垂直于)}参数来量化,这些参数是发现在300 nm处分别从-0.21和0.21变化到在313 nm处从-0.04和0.24变化。 (c)2006年美国物理研究所。

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