Belof Jonathan L, Brown Justin L, Myint Philip C, Sterbentz Dane M, Hao Yue, Stoltzfus Brian S, Benedict Lorin X
Lawrence Livermore National Laboratory, Livermore, CA 94550.
Sandia National Laboratories, Albuquerque, NM 87185.
Proc Natl Acad Sci U S A. 2025 May 20;122(20):e2424703122. doi: 10.1073/pnas.2424703122. Epub 2025 May 14.
Using pulsed-power magnetic field sources to compress gallium to gigapascal pressures on nanosecond timescales, we report here experiments on shockless dynamic compression of a liquid metal. Time-resolved velocimetry data reveal signatures of rapid freezing from a metastable liquid state, and we demonstrate that the kinetics of this nonequilibrium solidification can be accurately simulated with a computational modeling framework we have developed in previous studies, where classical nucleation theory is coupled with hydrodynamics. Notably, velocity traces in some of our experiments show evidence of a phase transition, while others do not, even though other types of evidence suggest that solidification may be occurring in all of them. We explain how predictions made by our models regarding the presence or absence of these phase-transition signatures motivated additional experiments that later confirmed the theoretical predictions. Our analysis shows that due to the rapid, quasi-isentropic nature of the loading path, our experiments were able to compress liquid gallium to metastable states that are undercooled below the equilibrium melt temperature by more than 300 K and exhibit pressures that approach five times the equilibrium melt pressure. The understanding gained in this study should form the basis for future dynamic-compression experiments aimed at interrogating melt curves at high pressures.
利用脉冲功率磁场源在纳秒时间尺度上将镓压缩至吉帕斯卡压力,我们在此报告关于液态金属无冲击动态压缩的实验。时间分辨测速数据揭示了从亚稳态液态快速凝固的特征,并且我们证明,这种非平衡凝固的动力学可以用我们在先前研究中开发的一个计算建模框架精确模拟,该框架将经典成核理论与流体动力学相结合。值得注意的是,我们的一些实验中的速度轨迹显示出相变的证据,而其他实验则没有,尽管其他类型的证据表明所有实验中可能都在发生凝固。我们解释了我们的模型对这些相变特征是否存在的预测如何推动了后续实验,这些实验后来证实了理论预测。我们的分析表明,由于加载路径的快速、准等熵性质,我们的实验能够将液态镓压缩至亚稳态,这些亚稳态的过冷度低于平衡熔化温度超过300 K,并且压力接近平衡熔化压力的五倍。本研究中获得的认识应为未来旨在探究高压下熔化曲线的动态压缩实验奠定基础。