- Open Access
Surface freezing of water
© The Author(s). 2016
- Received: 5 November 2015
- Accepted: 20 April 2016
- Published: 16 May 2016
Freezing, melting, evaporation and condensation of water are essential ingredients for climate and eventually life on Earth. In the present work, we show how surface freezing of supercooled water in an open container is conditioned and triggered—exclusively—by humidity in air. Additionally, a change of phase is demonstrated to be triggered on the water surface forming surface ice crystals prior to freezing of bulk. The symmetry of the surface crystal, as well as the freezing point, depend on humidity, presenting at least three different types of surface crystals. Humidity triggers surface freezing as soon as it overpasses a defined value for a given temperature, generating a plurality of nucleation nodes. An evidence of simultaneous nucleation of surface ice crystals is also provided.
- Surface Crystal
- Freezing Point
- Supercooled Water
- Open Container
- Surface Freezing
Nakaya demonstrated that snow crystals grow in cold humid air as a large variety of mainly plane crystals depending on both temperature and humidity of air 80 years ago (Magono and Woo 1966). As they were formed by inverse sublimation from vapor nobody got surprised that humidity—i.e. water vapor concentration in air—had a role on the kind of crystal grown. Up to 35 meteorological groups were described. More recently this number has grown up to 121 categories (Kikuchi et al. 2013).
More recently 2D confined water and ice crystals have attracted the attention of researchers. They are described to appear between two solid layers (Chen et al. 2015) with a structure depending on pressure and width (Zangi and Mark 2003). Molecular dynamics simulations show multiple possible structures of water confined between parallel bonding walls: dodecagonal quasicrystal bilayers (Johnston et al. 2010), ferroelectric hexagonal monolayers, rhombic monolayers (Zhao et al. 2014) and room temperature square ice (Algara-Siller et al. 2015). Additionally, some structural similarities between supercooled water and confined ice layers have also recently been described (Ricci et al. 2009). Particularly first neighboring oxygens and H-bonds in supercooled water and confined ice are both shorter than in common water or unconfined ice.
Hydrophobicity and hydrophilicity of surfaces confining liquid water seem to modulate its density at the nano-scale (Giovambattista et al. 2007), presenting a larger diffusivity when confined in mesopores by hydrophobic surfaces (Aso et al. 2012) and additionally “ab initio” computations demonstrate a phase change in nano-confined ice from a honeycomb to square under pressure depending on the hydrophobicity/hydrophilicity of such surfaces (Corsetti et al. 2016).
In previous works we demonstrated that humidity strongly affected surface energy, i.e. surface tension, (Pérez-Díaz et al. 2012) of water as well the freezing point of supercooled water droplets (Pérez-Díaz et al. 2015; Perez-Diaz et al. 2016). Moreover, the formation of icicles protruding from droplets suggested that surface freezing preceded bulk freezing.
However, it remained unknown whether it was a phenomenon associated to the liquid water–air interface or to the size and shape of the droplets used in those experiments. Moreover, it was no clear how freezing progressed into the bulk or if a truly surface crystallization occurred. In the present work, we aim to answer these two last questions performing new experiments with deionized water in open containers. The liquid water–air interface in these containers is perfectly flat except for the border in contact with their walls.
Figure 5 and the corresponding video show an interesting case in which two Surface single crystals are nucleated almost simultaneously (within the 40 ms time interval between successive frames). The different apparent growth kinetics of the right branch seem to be caused by the curvature of the surface due to the surface tension and the proximity of the edge.
The experiments described in the present paper demonstrate that the dependence of the freezing point of deionized water on humidity in air is intrinsic to the existence of the liquid water–air interface. The freezing temperature-humidity curves for open containers and for droplets are the same. For a given temperature, surface freezing is nucleated at the liquid water–air interface by a high enough humidity, forming a surface ice crystal prior to freezing of bulk. The symmetry of the surface crystal, as well as the freezing point, depend on humidity, presenting at least three different types of surface crystals. An evidence of simultaneous nucleation of Surface ice single crystals is also provided.
JLPD proposed, designed and coordinated the experiment, analysed data and proposed the physical interpretation. MAAV designed and built the hardware and collected and processed data. FRC carried out the sets of experiments. All authors read and approved the final manuscript.
This work has been supported by MAG SOAR SL.
The authors declare that they have no competing interests.
Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
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