Noguchi Naoki, Komatsu Kazuki, Shinozaki Ayako, Shinoda Keiji, Kagi Hiroyuki
Geochemical Research Center, Graduate School of Science, The University of Tokyo, Hongo, Bunkyo-ku, Tokyo 113-0033, Japan.
Geochemical Research Center, Graduate School of Science, The University of Tokyo, Hongo, Bunkyo-ku, Tokyo 113-0033, Japan.
Spectrochim Acta A Mol Biomol Spectrosc. 2014 Dec 10;133:509-13. doi: 10.1016/j.saa.2014.06.024. Epub 2014 Jun 18.
The nature of protons in ice VII up to 368°C and 16GPa was investigated with synchrotron near-infrared spectroscopy. The absorption band of the first OH stretching overtone mode divided into doublet peaks above 5GPa at room temperature, suggesting that proton tunneling occurs at the overtone level. As the temperature increased, the doublet peaks gradually reduced to a singlet. This result implies that thermally activated protons hop between the two potential minima along the oxygen-oxygen axis. A pressure-temperature diagram for the proton state was constructed from the changing band shape of the overtone mode.
利用同步加速器近红外光谱研究了高达368°C和16GPa压力下冰VII中质子的性质。在室温下,当压力高于5GPa时,第一个OH伸缩倍频模式的吸收带分裂为双峰,这表明质子隧穿发生在倍频水平。随着温度升高,双峰逐渐合并为单峰。该结果表明,热激活的质子沿氧-氧轴在两个势阱之间跳跃。根据倍频模式变化的能带形状构建了质子态的压力-温度图。