Lin Jung-Fu, Militzer Burkhard, Struzhkin Viktor V, Gregoryanz Eugene, Hemley Russell J, Mao Ho-kwang
Geophysical Laboratory, Carnegie Institution of Washington, Washington, DC 20015, USA.
J Chem Phys. 2004 Nov 1;121(17):8423-7. doi: 10.1063/1.1784438.
The melting curve of H(2)O has been measured by in situ Raman spectroscopy in an externally heated diamond anvil cell up to 22 GPa and 900 K. The Raman-active OH-stretching bands and the translational modes of H(2)O as well as optical observations are used to directly and reliably detect melting in ice VII. The observed melting temperatures are higher than previously reported x-ray measurements and significantly lower than recent laser-heating determinations. However, our results are in accord with earlier optical determinations. The frequencies and intensities of the OH-stretching peaks change significantly across the melting line while the translational mode disappears altogether in the liquid phase. The observed OH-stretching bands of liquid water at high pressure are very similar to those obtained in shock-wave Raman measurements.
利用外部加热的金刚石对顶砧细胞,通过原位拉曼光谱在高达22吉帕斯卡和900开尔文的条件下测量了H₂O的熔化曲线。利用拉曼活性的OH伸缩带、H₂O的平移模式以及光学观测来直接且可靠地检测冰VII中的熔化。观测到的熔化温度高于先前报道的X射线测量结果,且显著低于近期激光加热测定的结果。然而,我们的结果与早期的光学测定结果一致。OH伸缩峰的频率和强度在熔化线上有显著变化,而平移模式在液相中完全消失。在高压下观测到的液态水的OH伸缩带与冲击波拉曼测量中获得的非常相似。