Quasi-isentropic compression of liquid water beyond 5 GPa rapidly creates ice VII on 1–10 ns time scales. The onset of this phase transition can be modified by changing the initial temperature of… Click to show full abstract
Quasi-isentropic compression of liquid water beyond 5 GPa rapidly creates ice VII on 1–10 ns time scales. The onset of this phase transition can be modified by changing the initial temperature of the liquid sample and/or the compression rate. These effects were studied using the Sandia Thor-64 pulsed power machine. Increasing the initial temperature pushes freezing above the previously reported 7 GPa metastable limit. Slower compression allows freezing to occur below the metastable limit, though the compression rate has a greater effect at an elevated temperature than at room temperature.Quasi-isentropic compression of liquid water beyond 5 GPa rapidly creates ice VII on 1–10 ns time scales. The onset of this phase transition can be modified by changing the initial temperature of the liquid sample and/or the compression rate. These effects were studied using the Sandia Thor-64 pulsed power machine. Increasing the initial temperature pushes freezing above the previously reported 7 GPa metastable limit. Slower compression allows freezing to occur below the metastable limit, though the compression rate has a greater effect at an elevated temperature than at room temperature.
               
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