圧迫下での大量超冷却水における液体-液体移行の実験観察
Kyung Hwan Kim1,2, Katrin Amann-Winkel1, Nicolas Giovambattista3,4
1Department of Physics, AlbaNova University Center, Stockholm University, SE-10691 Stockholm, Sweden.
まとめ
研究者たちは 超冷却された水で 液体から液体への移行を 観測しました アモルフな氷の超高速加熱により,結晶化前に形成された明確な低密度ドメインが明らかになり,この相変化をサポートしました.
科学分野:
- 物理化学
- 凝縮物質物理学
- 材料科学
背景:
- 超冷却された水は 圧力と温度が異なる条件下で 複雑な振る舞いを表します
- 水の相変化を理解することは,様々な科学分野にとって極めて重要です.
研究 の 目的:
- 圧力の下にある超冷却水の大量の構造的動態を調査する.
- 液体と液体の相変化の証拠を 提供するためです
主な方法:
- フェムト秒レーザーを用いて高密度の無形氷のイソコリック加熱
- フェムト秒のX線レーザーパルスによる超高速構造分析
- ナノ秒からマイクロ秒のスケールで解圧と構造の変化をモニターします.
主要な成果:
- 高密度の液体水は205Kと2.5-3.5kbarで調製された.
- 低密度の液体領域が現れ,増加した.
- 結晶化はドメイン形成から分離したより長い時間スケール (3〜50マイクロ秒) で発生した.
結論:
- 観測された時間スケールの分離は,超冷却された水における液体-液体の移行を支持する.
- フェムト秒のX線 difraktionは,水中の超高速の相変化を研究するための強力なツールです.
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