立方氷の形成は,地球の大気に関係する条件下で形成される
Benjamin J Murray1, Daniel A Knopf, Allan K Bertram
1Department of Chemistry, University of British Columbia, 2036 Main Mall, Vancouver, British Columbia V6T 1Z1, Canada.
Nature
|March 11, 2005
まとめ
実験室での実験では,190K以下で凍結する純粋な水滴から立方体氷が形成されていることが示されています.この発見は,大気中の氷雲とその地球気候への潜在的な影響を理解するために不可欠です.
科学分野:
- 大気化学 大気化学
- クリスタログラフィーです.
- 地質物理学 地質物理学とは地質物理学です.
背景:
- 大気中の水滴の氷の均質な核化は,通常六角氷を形成します.
- 以前の報告では,地球の大気圏で立方形の氷が形成される可能性を示唆しています.
研究 の 目的:
- 空気の条件下で,純粋な水と水溶液滴で立方体の氷の形成を調査する.
- 温度範囲と立方体氷の形成を好む条件を決定する.
主な方法:
- マイクロメートルの水滴の均質な核化を含む実験室での実験.
- 大気条件を模倣した制御された冷却速度.
- 氷結晶相形成の分析. 氷結晶相形成の分析.
主要な成果:
- 立方形の氷の形成は,純粋な水と水溶液の滴が均質に凍結しているのに観察されました.
- 立方形の氷の形成は,190K以下の温度で優位である.
- この温度範囲は,極地層の平流層雲と熱帯の熱帯層雲に当てはまります.
結論:
- 立方体の氷は,特定の条件下で地球の大気中に形成されます.
- 立方体の氷の存在は,雲の微物理,水蒸気圧,氷粒子の大きさの分布を変化させる可能性があります.
- これは,トロポパウズ領域での脱水の増加につながる可能性があります.
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