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  • 1
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    Unknown
    MDPI - Multidisciplinary Digital Publishing Institute
    Publication Date: 2023-12-20
    Description: Ice crystals are the most ubiquitous material found in the cryosphere environment of the Earth, in the planetary system, and also in our daily lives. In recent years, ice crystals have increased in importance as one of the key materials for finding solutions to settle various environmental concerns at a global scale. Furthermore, ice crystals are unique materials which are potentially extremely useful in various applications, for example, within the food sciences, medical sciences, and other fields. In dealing with these interesting subjects, research on ice crystals has been more actively pursued in recent years. The Special Issue “Ice Crystals” presents a wide varieties of topics related to ice crystals. It can be considered as a status report reviewing the recent research on ice crystals and serves to provide readers with information on the latest developments concerning ice crystals.
    Keywords: Q1-390 ; QC1-999 ; coarsening kinetics ; antifreeze protein ; microstructure ; ice crystals ; decomposition ; formation ; cryo-photo microscopy ; cryoprotective agent ; ice cream ; reformation ; tomography ; deformation ; clathrate hydrate ; Negative thermal expansivity ; tetrahydrofuran ; ice crystal ; pressure ; molecular dynamics ; Grüneisen parameter ; modelling ; ab initio calculation ; freezing ; nanoscale pores ; quasi-liquid layer ; electron paramagnetic resonance ; potential of mean force ; gas hydrate ; spin labeling ; pre-decomposition pressure ; mW model ; bic Book Industry Communication::G Reference, information & interdisciplinary subjects::GP Research & information: general
    Language: English
    Format: application/octet-stream
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  • 2
    Publication Date: 2018-04-23
    Description: Ice-binding proteins (IBPs), produced by polar and cold-tolerant organisms, have the ability to bind to ice, affecting its growth. They are key elements in biological adaptation to cold environments, and no other particles, either natural nor synthetic, show a comparable effect in controlling ice growth. Here we present the IBPs from the polar sea-ice diatom Fragilariopsis cylindrus (fcIBP). This protein can shape the ice and allows survival of the diatom within sea-ice. It belongs to a protein family defined by a domain (DUF 3494) that is extremely successful among marine polar microorganisms but is also identified in other habitats such as, for example, an Antarctic ice-core. In order to shed light on the details of the interaction between IBPs and ice, as a first step leading to a better understanding of the effect of the proteins in their natural icy environment, we studied the effects of fcIBPs on single crystal free growth. Different IBP families affect ice in different ways and the relevant common traits, as well as the differences of the ice binding mechanisms, are still under investigation. We analyzed crystal morphological changes and crystal growth rates dependent on supercooling and fcIBP concentration, applying optical bright field and interferometric microscopy. We saw differential effects of the protein on the growth of the different crystallographic planes, revealing a new pattern of IBP–ice interaction. Furthermore, switching to a more macroscopic level, we analyzed the effect of fcIBPs on the physical properties of polycrystalline ice. We observed the evolution of microstructure in fine-grained ice samples over longer time periods (several weeks), and were able to show a strong inhibition by fcIBPs of grain growth. Also, we showed that the effect of IBPs on the driving factors for ice deformation during creep, i.e. on internal dislocations due to incorporation within the lattice and on the mobility of grain boundaries due to pinning, make these proteins particularly interesting in studying the process of ice deformation. Our results of ice single crystal growth and of the microstructure evolution of polycrystalline ice in the presence of fcIBPs show that these proteins have remarkable properties that make them suited to basic understanding of the mechanisms of grain growth, recrystallization and deformation processes, but also to be adapted for industrial applications wherever ice grain control is of interest.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 3
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    Unknown
    In:  EPIC314th International Conference on the Physics and Chemistry of Ice (PCI), Zürich (Switzerland), 2018-01-07-2018-01-12
    Publication Date: 2018-04-23
    Description: Ice-binding proteins (IBPs), produced by polar and cold-tolerant organisms, have the ability to bind to ice, affecting its growth. They are key elements in biological adaptation to cold environments, and no other particles, neither natural nor synthetic, show comparable effect in controlling ice growth. However, the details of the protein-ice interactions have not been clarified yet. Different IBP families affect ice in different ways, and the relevant common traits, as well as the differences of the ice binding mechanisms, are still under investigation. Here we present the IBP from the polar sea-ice diatom Fragilariopsis cylindrus (fcIBP). It belongs to a protein family defined by a domain (DUF 3494) extremely successful among polar microorganisms. We studied the effects of the fcIBPs on single crystal free growth using optical bright field and interferometric microscopy. We studied crystal morphology changes and growth rates dependent on supercooling and protein concentration. We saw differential effects of the protein on the growth of crystallographic planes, dependent on fcIBP dynamics in the different directions. We relate this to differential affinity and adsorption time of the protein to the basal and prismatic planes. Switching to a more macroscopic level, we analyzed the effect of the proteins to physical properties of polycrystalline ice. We observed the evolution of microstructure in fine-grained samples over several weeks and we show the strong inhibition of fcIBPs on grain growth. We further show that the effect of fcIBPs on the driving factors for ice deformation during creep, i.e. on internal dislocations due to incorporation within the lattice and on the mobility of grain boundaries due to pinning, make these proteins particularly interesting for understanding basic processes of ice deformation.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 4
    facet.materialart.
    Unknown
    American Chemical Society
    In:  EPIC3Crystal Growth & Design, American Chemical Society, 18, pp. 2563-2571
    Publication Date: 2018-04-23
    Description: The morphology and growth kinetics of ice single crystals in aqueous solutions of type III antifreeze protein (AFP-III) have been studied in detail over a range of AFP-III concentrations and supercoolings. In pure water, the shape of ice crystals changes from the circular disklike to planar dendritic with increasing supercooling. In AFP-III solutions, ice crystals in the form of faceted plates, irregular dendrites with polygonized tips, and needles appear with increasing supercooling and AFP-III concentration. The growth rate of ice crystals in the crystallographic a direction is 2 orders of magnitude higher than that in the c direction. AFP-III molecules cause the stoppage of the growth of the prismatic and basal faces at low supercoolings. When supercooling exceeds the critical value, AFP-III favors the acceleration of the growth in both a and c directions. The observed behavior of AFP-III is explained in terms of the Cabrera-Vermilyea pinning model and the specificity of the dissipation of latent heat from the growing crystals with different shapes.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 5
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    NATL ACAD SCIENCES
    In:  EPIC3Proceedings of the National Academy of Sciences of the United States of America, NATL ACAD SCIENCES, 115(29), pp. 7479-7484, ISSN: 0027-8424
    Publication Date: 2018-07-30
    Description: Ice-binding proteins (IBPs) affect ice crystal growth by attaching to crystal faces. We present the effects on the growth of an ice single crystal caused by an ice-binding protein from the sea ice microalga Fragilariopsis cylindrus (fcIBP) that is characterized by the widespread domain of unknown function 3494 (DUF3494) and known to cause a moderate freezing point depression (below 1 °C). By the application of interferometry, bright-field microscopy, and fluorescence microscopy, we observed that the fcIBP attaches to the basal faces of ice crystals, thereby inhibiting their growth in the c direction and resulting in an increase in the effective supercooling with increasing fcIBP concentration. In addition, we observed that the fcIBP attaches to prism faces and inhibits their growth. In the event that the effective supercooling is small and crystals are faceted, this process causes an emergence of prism faces and suppresses crystal growth in the a direction. When the effective supercooling is large and ice crystals have developed into a dendritic shape, the suppression of prism face growth results in thinner dendrite branches, and growth in the a direction is accelerated due to enhanced latent heat dissipation. Our observations clearly indicate that the fcIBP occupies a separate position in the classification of IBPs due to the fact that it suppresses the growth of basal faces, despite its moderate freezing point depression.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
    Format: application/pdf
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  • 6
    Publication Date: 2017-08-28
    Description: Ice-binding proteins from the sea-ice microalgae Fragilariopsis cylindrus (fcIBPs) belong to a protein family widely spread among several organisms, from sea-ice microorganisms to cold-tolerant fungi. Their mechanism of action, the interaction with ice crystals and their influence on ice growth, differs from the one observed for fish or hyperactive AFPs. In order to understand the attachment process of fcIBPs we observed free growth of one ice single crystal from the melt. We present a new growth pattern of ice in the presence of IBPs. We used bright field microscopy and Mach-Zehnder interferometry to determine crystal morphology and growth rates parallel and normal to the basal plane. We corroborated our observations by fluorescence microscopy using the fcIBP fused to a fluorescent protein. Our results all indicated that fcIBPs bind preferentially to the basal plane, and to a less degree to some prismatic plane of the ice crystal. Whereas the observed strong suppression of growth normal to the basal plane was expected as directly reflected by morphology observations, ice growth enhancement by fcIBPs in direction of the basal plane, never observed before in other IBP kinds, was surprising. Set in a natural frame, the proteins, expelled from the microorganisms in the brine space primarily located between the basal planes of elongated crystals of columnar sea ice, may be helpful in maintaining a liquid environment by strongly controlling ice growth on the basal plane.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 7
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Chemie in unserer Zeit 31 (1997), S. 102-102 
    ISSN: 0009-2851
    Keywords: Chemistry ; Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Chemie in unserer Zeit 31 (1997), S. 58-65 
    ISSN: 0009-2851
    Keywords: Chemistry ; Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Snow crystals grown during their fall from water vapor in clouds are often witnessed with their fascinating beautiful patterns. How are these beautiful patterns created in nature? Recent theoretical and experimental advances in the understanding of the formation mechanism of snow crystals are explained on the basis of crystal growth.
    Notes: Eine selbstgebaute Schneehütte mit einer Mikroskop- und Kameraausrüstung im Inneren dient Y. Furukawa als „wohltemperiertes“ Labor zur Untersuchung von Schneekristallen. Hier entstanden auch die in Abbildung 1 gezeigten Mikrophotographien.
    Additional Material: 10 Ill.
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2016-02-01
    Description: Surfaces of ice are covered with thin liquid water layers, called quasi-liquid layers (QLLs), even below their melting point (0 °C), which govern a wide variety of phenomena in nature. We recently found that two types of QLL phases appear that exhibit different morphologies (droplets and thin layers) [Sazaki G. et al. (2012) Proc Natl Acad Sci USA 109(4):1052−1055]. However, revealing the thermodynamic stabilities of QLLs remains a longstanding elusive problem. Here we show that both types of QLLs are metastable phases that appear only if the water vapor pressure is higher than a certain critical supersaturation. We directly visualized the QLLs on ice crystal surfaces by advanced optical microscopy, which can detect 0.37-nm-thick elementary steps on ice crystal surfaces. At a certain fixed temperature, as the water vapor pressure decreased, thin-layer QLLs first disappeared, and then droplet QLLs vanished next, although elementary steps of ice crystals were still growing. These results clearly demonstrate that both types of QLLs are kinetically formed, not by the melting of ice surfaces, but by the deposition of supersaturated water vapor on ice surfaces. To our knowledge, this is the first experimental evidence that supersaturation of water vapor plays a crucially important role in the formation of QLLs.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 10
    Publication Date: 2018-07-02
    Description: Ice-binding proteins (IBPs) affect ice crystal growth by attaching to crystal faces. We present the effects on the growth of an ice single crystal caused by an ice-binding protein from the sea ice microalga Fragilariopsis cylindrus (fcIBP) that is characterized by the widespread domain of unknown function 3494 (DUF3494) and known to cause a moderate freezing point depression (below 1 °C). By the application of interferometry, bright-field microscopy, and fluorescence microscopy, we observed that the fcIBP attaches to the basal faces of ice crystals, thereby inhibiting their growth in the c direction and resulting in an increase in the effective supercooling with increasing fcIBP concentration. In addition, we observed that the fcIBP attaches to prism faces and inhibits their growth. In the event that the effective supercooling is small and crystals are faceted, this process causes an emergence of prism faces and suppresses crystal growth in the a direction. When the effective supercooling is large and ice crystals have developed into a dendritic shape, the suppression of prism face growth results in thinner dendrite branches, and growth in the a direction is accelerated due to enhanced latent heat dissipation. Our observations clearly indicate that the fcIBP occupies a separate position in the classification of IBPs due to the fact that it suppresses the growth of basal faces, despite its moderate freezing point depression.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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