Ice structures such as accretion on airplanes, wires, or roadways; ice falls; ice stalactites; frozen rivers; and aufeis are formed by the freezing of capillary flows (drops, rivulets, and films). To understand these phenomena, a detailed exploration of the complex coupling between capillary flow and solidification is necessary. Among the many scientific questions that remain open in order to understand these problems are the confinement of the thermal boundary layer by the free surface, the interaction between a freezing front and a free surface, the effect of freezing on the contact line motion, etc. This review focuses mainly on water and ice, discussing the theoretical framework and recent developments in the main areas of the freezing–capillarity interaction. The text deeply explores the freezing of a moving drop or a rivulet and the fundamental problem of wetting water on ice. Additionally, it highlights some of the main open questions on the subject.

中文翻译：

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 冻结和毛细作用


冰结构，例如飞机、电线或道路上的吸积物;冰瀑;冰钟乳石;结冰的河流;和 aufeis 是由毛细管流（液滴、小溪和薄膜）冻结形成的。为了理解这些现象，有必要详细探索毛细管流动和凝固之间的复杂耦合。为了理解这些问题，许多科学问题仍然存在，其中包括自由表面对热边界层的限制、冻结前沿和自由表面之间的相互作用、冻结对接触线运动的影响等。本文主要关注水和冰，讨论了冻结-毛细作用主要领域的理论框架和最新进展。文本深入探讨了移动的水滴或小溪的冻结以及在冰上润湿水的基本问题。此外，它还强调了有关该主题的一些主要开放性问题。