Abnormal gas-liquid-solid phase transition behaviour of water observed with in situ environmental SEM.
Ontology highlight
ABSTRACT: Gas-liquid-solid phase transition behaviour of water is studied with environmental scanning electron microscopy for the first time. Abnormal phenomena are observed. At a fixed pressure of 450?Pa, with the temperature set to -7?°C, direct desublimation happens, and ice grows continuously along the substrate surface. At 550?Pa, although ice is the stable phase according to the phase diagram, metastable liquid droplets first nucleate and grow to ~100-200??m sizes. Ice crystals nucleate within the large sized droplets, grow up and fill up the droplets. Later, the ice crystals grow continuously through desublimation. At 600?Pa, the metastable liquid grows quickly, with some ice nuclei floating in it, and the liquid-solid coexistence state exists for a long time. By lowering the vapour pressure and/or increasing the substrate temperature, ice sublimates into vapour phase, and especially, the remaining ice forms a porous structure due to preferential sublimation in the concave regions, which can be explained with surface tension effect. Interestingly, although it should be forbidden for ice to transform into liquid phase when the temperature is well below 0?°C, liquid like droplets form during the ice sublimation process, which is attributed to the surface tension effect and the quasiliquid layers.
SUBMITTER: Chen X
PROVIDER: S-EPMC5402395 | biostudies-literature | 2017 Apr
REPOSITORIES: biostudies-literature
ACCESS DATA