Quasi-liquid layers on ice crystal surfaces are made up of two different phases.
Ice plays crucially important roles in various phenomena because of its abundance on Earth. However, revealing the dynamic behavior of quasi-liquid layers (QLLs), which governs the surface properties of ice crystals at temperatures near the melting point, remains an experimental challenge. Here we show that two types of QLL phases appear that exhibit different morphologies and dynamics. We directly visualized the two types of QLLs on ice crystal surfaces by advanced optical microscopy, which can visualize the individual 0.37-nm-thick elementary steps on ice crystal surfaces. We found that they had different stabilities and different interactions with ice crystal surfaces. The two immiscible QLL phases appeared heterogeneously, moved around, and coalesced dynamically on ice crystal surfaces. This picture of surface melting is quite different from the conventional picture in which one QLL phase appears uniformly on ice crystal surfaces.
Institute of Low Temperature Science, Hokkaido University, N19-W8, Kita-ku, Sapporo 060-0819, Japan. sazaki@lowtem.hokudai.ac.jp
Gen
G
Sazaki
Salvador
S
Zepeda
Shunichi
S
Nakatsubo
Makoto
M
Yokomine
Yoshinori
Y
Furukawa
D007053:Ice / Q000032:analysis*; D018613:Microscopy, Confocal / Q000379:methods*; D008857:Microscopy, Interference / Q000379:methods*; D019370:Observation; D044367:Phase Transition; D014867:Water / Q000737:chemistry*
D007053:Ice; D014867:Water