Schmeisser Marcus, Iglev Hristo, Laubereau Alfred
Physik-Department E 11, Technische Universität München, D-85748 Garching, Germany.
J Phys Chem B. 2007 Sep 27;111(38):11271-5. doi: 10.1021/jp0736802. Epub 2007 Sep 5.
The ice-water phase transition after an ultrafast temperature jump is studied in HDO:D2O (15 M) ice with use of 2-color IR spectroscopy. The OH-stretching vibration is applied for rapid heating of the sample and for fast and sensitive probing of local temperature and structure. For energy depositions beyond the limit of superheating (330 +/- 10 K) partial melting in two steps is observed and assigned to (i) catastrophic melting within the thermalization time of the excited ice lattice of 5 +/- 2 ps and (ii) secondary melting with a time constant of 33 +/- 5 ps that is assigned to interfacial melting at the generated phase boundaries. The latter process is found to consume energy amounts in agreement with the latent heat of melting and is accompanied by an accelerated temperature and pressure decrease of the residual ice component.
利用双色红外光谱研究了超快温度跃变后HDO:D2O(15 M)冰中的冰水相变。OH伸缩振动用于样品的快速加热以及局部温度和结构的快速灵敏探测。对于超过过热极限(330±10 K)的能量沉积,观察到两步部分熔化,并归因于:(i)在激发冰晶格热化时间5±2 ps内的灾难性熔化;(ii)时间常数为33±5 ps的二次熔化,这归因于在生成的相界处的界面熔化。发现后一过程消耗的能量与熔化潜热一致,并伴随着残余冰成分温度和压力的加速下降。