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Investigations of structural and dynamical mechanisms of ice formation regulated by graphene oxide nanosheets

Recent research indicates that graphene oxide (GO) nanosheets can be used to regulate ice formation by controlling critical ice nucleus growth in water at supercooling temperatures. In addition, the study of ice formation mechanisms regulated by GO nanosheets, a good model system for antifreeze prot...

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Detalles Bibliográficos
Autores principales: Zhang, Shengkai, Han, Jingjing, Luo, Xiang, Wang, Zhixin, Gu, Xudong, Li, Na, de Souza, Nicolas R., Garcia Sakai, Victoria, Chu, Xiang-Qiang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Crystallographic Association 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8443304/
https://www.ncbi.nlm.nih.gov/pubmed/34549075
http://dx.doi.org/10.1063/4.0000111
Descripción
Sumario:Recent research indicates that graphene oxide (GO) nanosheets can be used to regulate ice formation by controlling critical ice nucleus growth in water at supercooling temperatures. In addition, the study of ice formation mechanisms regulated by GO nanosheets, a good model system for antifreeze proteins (AFPs), will shed light on how AFPs regulate ice formation in nature. In this work, time-resolved small-angle x-ray scattering (TR-SAXS) and quasi-elastic neutron scattering (QENS) experiments were carried out to investigate the structural and dynamical mechanisms of ice formation regulated by GO nanosheets. Strikingly, a transient intermediate state was observed in TR-SAXS experiments that only exists in the aqueous dispersions with a larger GO size (11 nm). This serves as evidence that the size of GO is critical for regulating ice formation. Elastic neutron scattering results indicate that ice is formed in all samples and thermal hysteresis occurs in GO aqueous dispersions in both H(2)O and D(2)O. The structural and dynamics information about water molecules in GO, extracted from QENS, reveals different dynamical behaviors of water molecules in GO aqueous dispersions when approaching the ice formation temperature.