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Isotope effects in liquid water probed by transmission mode x-ray absorption spectroscopy at the oxygen K-edge

机译:通过透射模式X射线吸收光谱在氧气K边缘探测液态水中的同位素效应

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The effects of isotope substitution in liquid water are probed by x-ray absorption spectroscopy at the O K-edge as measured in transmission mode. Confirming earlier x-ray Raman scattering experiments, the D2O spectrum is found to be blue shifted with respect to H2O, and the D2O spectrum to be less broadened. Following the earlier interpretations of UV and x-ray Raman spectra, the shift is related to the difference in ground-state zero-point energies between D2O and H2O, while the difference in broadening is related to the difference in ground-state vibrational zero-point distributions. We demonstrate that the transmission-mode measurements allow for determining the spectral shapes with unprecedented accuracy. Owing in addition to the increased spectral resolution and signal to noise ratio compared to the earlier measurements, the new data enable the stringent determination of blue shift and broadening in the O K-edge x-ray absorption spectrum of liquid water upon isotope substitution. The results are compared to UV absorption data, and it is discussed to which extent they reflect the differences in zero-point energies and vibrational zero-point distributions in the ground-states of the liquids. The influence of the shape of the final-state potential, inclusion of the Franck-Condon structure, and differences between liquid H2O and D2O resulting from different hydrogen-bond environments in the liquids are addressed. The differences between the O K-edge absorption spectra of water from our transmission-mode measurements and from the state-of-the-art x-ray Raman scattering experiments are discussed in addition. The experimentally extracted values of blue shift and broadening are proposed to serve as a test for calculations of ground-state zero-point energies and vibrational zero-point distributions in liquid H2O and D2O. This clearly motivates the need for new calculations of the O K-edge x-ray absorption spectrum of liquid water. Published by AIP Publishing.
机译:通过在透射模式下测量的O K边缘处的X射线吸收光谱,研究了液态水中同位素取代的影响。证实了较早的X射线拉曼散射实验,发现D2O光谱相对于H2O发生了蓝移,而D2O光谱的展宽范围较小。根据对UV和X射线拉曼光谱的早期解释,位移与D2O和H2O之间的基态零点能量的差异有关,而展宽的差异与基态振动零能级的差异有关。点分布。我们证明了传输模式的测量允许以前所未有的精度确定频谱形状。由于与以前的测量相比,除了光谱分辨率和信噪比提高之外,新数据还能够严格确定同位素取代后液态水的O边缘X射线吸收光谱中的蓝移和加宽。将结果与紫外线吸收数据进行比较,并讨论它们在多大程度上反映了液体基态中零点能量和振动零点分布的差异。讨论了最终状态电势的形状,弗兰克-康登结构的夹杂物以及由于液体中氢键环境不同而引起的液体H2O和D2O之间差异的影响。此外,我们还讨论了通过我们的传输模式测量和最新的X射线拉曼散射实验得出的水的O K边缘吸收光谱之间的差异。提出了实验提取的蓝移和展宽值,以作为计算液态H2O和D2O中的基态零点能量和振动零点分布的测试方法。显然,这激发了对液态水的O K边缘X射线吸收光谱进行新计算的需求。由AIP Publishing发布。

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