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Time-Lapse, in Situ Imaging of Ice Crystal Growth Using Confocal Microscopy
Author(s) -
Moreno Marcellini,
Cécile Noirjean,
Dmytro Dedovets,
Juliette Maria,
Sylvain Deville
Publication year - 2016
Publication title -
acs omega
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.779
H-Index - 40
ISSN - 2470-1343
DOI - 10.1021/acsomega.6b00217
Subject(s) - ice crystals , nucleation , crystal growth , materials science , in situ , crystal (programming language) , optical microscope , chemical physics , confocal , confocal laser scanning microscopy , morphology (biology) , microscopy , nanotechnology , crystallography , geology , optics , chemistry , biophysics , thermodynamics , computer science , scanning electron microscope , physics , composite material , biology , paleontology , programming language , organic chemistry
Ice crystals nucleate and grow when a water solution is cooled below its freezing point. The growth velocities and morphologies of the ice crystals depend on many parameters, such as the temperature of ice growth, the melting temperature, and the interactions of solutes with the growing crystals. Three types of morphologies may appear: dendritic, cellular (or fingerlike), or the faceted equilibrium form. Understanding and controlling which type of morphology is formed is essential in several domains, from biology to geophysics and materials science. Obtaining, in situ, three dimensional observations without introducing artifacts due to the experimental technique is nevertheless challenging. Here we show how we can use laser scanning confocal microscopy to follow in real-time the growth of smoothed and faceted ice crystals in zirconium acetate solutions. Both qualitative and quantitative observations can be made. In particular, we can precisely measure the lateral growth velocity of the crystals, a measure otherwise difficult to obtain. Such observations should help us understand the influence of the parameters that control the growth of ice crystals in various systems.

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