Osmotic-Pressure-Induced Nematic Ordering in Suspensions of Laponite and Carboxy Methyl Cellulose

dc.contributor.author Xu, Peicheng
dc.contributor.author Yazici, Ahmet F.
dc.contributor.author Erdem, Talha
dc.contributor.author Lekkerkerker, Henk N. W.
dc.contributor.author Mutlugun, Evren
dc.contributor.author Eiser, Erika
dc.contributor.authorID 0000-0003-2747-7856 en_US
dc.contributor.authorID 0000-0003-3905-376X en_US
dc.contributor.authorID 0000-0003-2881-8157 en_US
dc.contributor.department AGÜ, Mühendislik Fakültesi, Elektrik - Elektronik Mühendisliği Bölümü en_US
dc.date.accessioned 2021-01-25T11:38:30Z
dc.date.available 2021-01-25T11:38:30Z
dc.date.issued 2020 en_US
dc.description We thank the Winton Program for the Physics of Sustainability for financial support. T.E. and A.F.Y. thank the Royal Society for the Newton International Fellowship Alumni Follow-on Funding. E.E. thanks Daan Frenkel for insightful discussions and expresses her gratitude to Emily Carter, whose example shows that it is possible to be an outstanding scientist and at the same time an exceptional human being. en_US
dc.description.abstract Laponite is a synthetic clay that is known to form gels in aqueous suspensions at low concentrations (0.01 g/cm(3)) Although it is expected to form lyotropic liquid crystals, such phases usually do not form, as a consequence of laponite's tendency to form gels at concentrations below the threshold for liquid crystal formation. Here we show that macroscopic, birefringent phases of laponite can be prepared through osmotic compression of a laponite solution by an aqueous solution of carboxy methyl cellulose (CMC). We present polarization imaging studies showing how the initially dilute, isotropic laponite phase shrinks while developing typical birefringence colors between crossed polarizers. Using the MichelLevy interference charts, we were able to extract the refractive index and orientation of the laponite nanodisks in the compressed region. Our observations allow us to propose a tentative state diagram, indicating the concentration regions for which we obtain optically anisotropic gels. en_US
dc.description.sponsorship Winton Program for the Physics of Sustainability Royal Society of London en_US
dc.identifier.endpage 9481 en_US
dc.identifier.issn 1520-6106
dc.identifier.issn 1520-5207
dc.identifier.issue 42 en_US
dc.identifier.other PubMed ID: 33043670
dc.identifier.startpage 9475 en_US
dc.identifier.uri https://doi.org/10.1021/acs.jpcb.0c06674
dc.identifier.uri https://hdl.handle.net/20.500.12573/480
dc.identifier.volume Volume: 124 en_US
dc.language.iso eng en_US
dc.publisher AMER CHEMICAL SOC, 1155 16TH ST, NW, WASHINGTON, DC 20036 USA en_US
dc.relation.isversionof 10.1021/acs.jpcb.0c06674 en_US
dc.relation.journal JOURNAL OF PHYSICAL CHEMISTRY B en_US
dc.relation.publicationcategory Makale - Uluslararası - Editör Denetimli Dergi en_US
dc.rights info:eu-repo/semantics/closedAccess en_US
dc.subject PHASE-DIAGRAM en_US
dc.subject CLAY en_US
dc.subject GELS en_US
dc.subject CRYSTALS en_US
dc.subject BEHAVIOR en_US
dc.title Osmotic-Pressure-Induced Nematic Ordering in Suspensions of Laponite and Carboxy Methyl Cellulose en_US
dc.type article en_US

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