Frozen State of Sephadex ® Gels of Different Crosslink Density Analyzed by X-ray Computed Tomography and X-ray Diffraction

Water in Sephadex (crosslinked dextran) gels is known to indicate different freezing behavior which is dependent on the density of the crosslinks, and water in a Sephadex G25 gel remains partially unfrozen during cooling and crystallizes during rewarming. The mechanism of anomalous ice crystallizati...

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Bibliographic Details
Published in:Gels 2018-05, Vol.4 (2), p.44
Main Authors: Murase, Norio, Uetake, Yuki, Sato, Yuki, Irie, Kentaro, Ueno, Yohei, Hirauchi, Toru, Kawahara, Toshio, Hirai, Mitsuhiro
Format: Article
Language:English
Subjects:
Beads
Computation
Computed tomography
Cooling
Crosslinking
Crystallization
Density
Equilibrium
Food
Gels
Grains
Ice
Ice crystals
Ice formation
Medical imaging
Polymers
R&D
Research & development
Spectrum analysis
Synchrotron radiation
X-ray diffraction
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Summary:Water in Sephadex (crosslinked dextran) gels is known to indicate different freezing behavior which is dependent on the density of the crosslinks, and water in a Sephadex G25 gel remains partially unfrozen during cooling and crystallizes during rewarming. The mechanism of anomalous ice crystallization during rewarming is still unclear. The objective of this study is to observe the ice grains that form in Sephadex beads and to comprehend their frozen state with a focus on the ice crystallization during rewarming. Sephadex beads containing 50 wt % water were prepared and used for the measurements. The observation of the ice grains was carried out by using synchrotron radiation-sourced X-ray CT (computed tomography). XRD (X-ray diffraction) analysis was also conducted to investigate the frozen state. As a result, ice grains that were larger than ~1 μm were hardly observed after the slow cooling of Sephadex beads, except in the G25 beads. However, at the occurrence of ice crystallization during rewarming, ice grains that were larger than 10 μm appeared in the G25 beads. Using XRD, it was found that small incomplete ice crystals were formed in G25 beads and the presence of glassy water was indicated in the gel. In conclusion, the size and distribution of ice grains that formed in Sephadex beads were different depending on the density of the crosslinks.
ISSN:2310-2861
2310-2861
DOI:10.3390/gels4020044