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Vitrification and increase of basicity in between ice I-h crystals in rapidly frozen dilute NaCl aqueous solutions

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68081731%3A_____%2F19%3A00508177" target="_blank" >RIV/68081731:_____/19:00508177 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/00216224:14310/19:00108241

  • Výsledek na webu

    <a href="https://aip.scitation.org/doi/10.1063/1.5100852" target="_blank" >https://aip.scitation.org/doi/10.1063/1.5100852</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1063/1.5100852" target="_blank" >10.1063/1.5100852</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Vitrification and increase of basicity in between ice I-h crystals in rapidly frozen dilute NaCl aqueous solutions

  • Popis výsledku v původním jazyce

    The freezing of ionic aqueous solutions is common in both nature and human-conducted cryopreservation. The cooling rate and the dimensions constraining the solution are known to fundamentally influence the physicochemical characteristics of the sample, including the extent of vitrification, morphology, and distribution of ions. The presence of some salts in an aqueous solution often suppresses the ice crystallization, allowing bulk vitrification during relatively slow cooling. Such a process, however, does not occur in NaCl solutions, previously observed to vitrify only under hyperquenching and/or in sub-micrometric confinements. This work demonstrates that, at freezing rates of >= 100 K min(-1), crystallized ice I-h expels the freeze-concentrated solution onto the surfaces of the crystals, forming lamellae and veins to produce glass, besides eutectic crystallization. The vitrification covers (6.8% +/- 0.6%) and (17.9% +/- 1.5%) of the total eutectic content in 0.06M and 3.4 mM solutions, respectively. The vitrified solution shows a glass-to-liquid transition succeeded by cold crystallization of NaCl 2H(2)O during heating via differential scanning calorimetry. We establish that ice crystallization is accompanied by increased basicity in freeze-concentrated solutions, reflecting preferential incorporation of chloride anions over sodium cations into the ice. After the sample is heated above the glass transition temperature, the acidity gradually returns towards the original value. The morphology of the samples is visualized with an environmental scanning electron microscope. Generally, the method of vitrifying the freeze-concentrated solution in between the ice I-h crystals via fast cooling can be considered a facile route towards information on vitrified solutions.

  • Název v anglickém jazyce

    Vitrification and increase of basicity in between ice I-h crystals in rapidly frozen dilute NaCl aqueous solutions

  • Popis výsledku anglicky

    The freezing of ionic aqueous solutions is common in both nature and human-conducted cryopreservation. The cooling rate and the dimensions constraining the solution are known to fundamentally influence the physicochemical characteristics of the sample, including the extent of vitrification, morphology, and distribution of ions. The presence of some salts in an aqueous solution often suppresses the ice crystallization, allowing bulk vitrification during relatively slow cooling. Such a process, however, does not occur in NaCl solutions, previously observed to vitrify only under hyperquenching and/or in sub-micrometric confinements. This work demonstrates that, at freezing rates of >= 100 K min(-1), crystallized ice I-h expels the freeze-concentrated solution onto the surfaces of the crystals, forming lamellae and veins to produce glass, besides eutectic crystallization. The vitrification covers (6.8% +/- 0.6%) and (17.9% +/- 1.5%) of the total eutectic content in 0.06M and 3.4 mM solutions, respectively. The vitrified solution shows a glass-to-liquid transition succeeded by cold crystallization of NaCl 2H(2)O during heating via differential scanning calorimetry. We establish that ice crystallization is accompanied by increased basicity in freeze-concentrated solutions, reflecting preferential incorporation of chloride anions over sodium cations into the ice. After the sample is heated above the glass transition temperature, the acidity gradually returns towards the original value. The morphology of the samples is visualized with an environmental scanning electron microscope. Generally, the method of vitrifying the freeze-concentrated solution in between the ice I-h crystals via fast cooling can be considered a facile route towards information on vitrified solutions.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10403 - Physical chemistry

Návaznosti výsledku

  • Projekt

    <a href="/cs/project/GA19-08239S" target="_blank" >GA19-08239S: Spektroskopie a mikroskopie chemických látek v ledu pro environmentální a farmaceutické účely</a><br>

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2019

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Journal of Chemical Physics

  • ISSN

    0021-9606

  • e-ISSN

  • Svazek periodika

    151

  • Číslo periodika v rámci svazku

    1

  • Stát vydavatele periodika

    US - Spojené státy americké

  • Počet stran výsledku

    11

  • Strana od-do

    014503

  • Kód UT WoS článku

    000474214600023

  • EID výsledku v databázi Scopus

    2-s2.0-85068450375