熱工学コンファレンス講演論文集
Online ISSN : 2424-290X
セッションID: D214
会議情報
D214 固体・水界面での氷の核生成に対する接触面積の影響(OS-11:凝固・融解を伴う伝熱現象とその応用(4))
稲田 孝明富田 博之小山 寿恵
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会議録・要旨集 フリー

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To discuss the uniformity of ice nucleating activity of solid/water interfaces, ice nucleation in water droplets prepared on glass surfaces was investigated for various droplet sizes from micrometer to sub-millimeter. When the interfacial area between water and the glass surface was larger than 1×10^<-8> m^2, the ice nucleation temperature showed large scatter, suggesting that the ice nucleating activity was no longer uniform. When the classical nucleation theory (CNT) is used to analyze surface-induced ice nucleation, the uniformity of interfaces that contribute to ice nucleation must be carefully considered, because CNT cannot be directly applied to non-uniform interfaces.
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© 2013 一般社団法人 日本機械学会
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