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Thermotropic Liquid Crystal Developable Domains in This and Similar Systems

dc.contributor.authorRamos Riesco, Miguel
dc.contributor.authorMartínez Casado, Francisco J.
dc.contributor.authorRodríguez Ched, José A.
dc.contributor.authorRedondo Yélamos, María Isabel
dc.contributor.authorFernandez Martínez,, Alejandro
dc.contributor.authorLópez De Andrés, María Sol
dc.date.accessioned2023-06-18T06:04:01Z
dc.date.available2023-06-18T06:04:01Z
dc.date.issued2015-11
dc.description.abstractA new third polymorph of copper(II) decanoate has been found by two methods: from the crystallization of the salt−acid solution and from a specific thermal treatment of the polymorph obtained in n-heptane. The new polymorph, whose crystal structure has been solved for the first time, is the most stable from the thermodynamic point of view. It presents a bilayer structure, but with two different types of paddle-wheels catenae with opposite orientations. This polymorphism as well as the temperature vs composition phase diagram of the system, [(1−x) C9H21CO2H + (x) (C9H21CO2)2Cu], was solved by differential scanning calorimetry, Fourier transform infrared spectroscopy, X-ray diffraction, pair distribution function, and optical microscopy. The singularities of the phase diagram are (a) a Krafft-like process of molecular association of the copper(II) decanoate into the acid solution, at about T = 361.5 K and x = 0.022 (forming salt-acid adducts of 1:1 stoichiometry); (b) a fusion transition as an invariant (T = 379.1 K) of the solid salt in excess from the copper(II) decanoate crystal phase to the discotic liquid crystal, forming homeotropic developable domains (seen for the first time in these systems) of the pure salt into the saturated acid solution. These domains are seen not only in the copper(II) decanoate but also in other members of the series, at high salt concentration in the corresponding acid solution, and allow identification of the hexagonal columnar discotic structure of the mesophase (with the exception of the copper(II) butanoate, where the tetragonal domains with tilted disks, paddle-wheels, were seen in the same salt−acid region).
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Educación y Ciencia
dc.description.sponsorshipUniversidad Complutense de Madrid
dc.description.sponsorshipEuropean Synchrotron Radiation Facility (ESRF). Grenoble
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/62277
dc.identifier.doihttps:// 10.1021/cg501572s
dc.identifier.issnIssn: 1528-7483 ; Essn: 1528-7505
dc.identifier.officialurlhttps://pubs.acs.org/toc/cgdefu/15/1
dc.identifier.relatedurlhttps://pubs.acs.org/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/23833
dc.issue.number1
dc.journal.titleCrystal growth & design
dc.language.isoeng
dc.page.final509
dc.page.initial497
dc.publisherAmerican Chemical Society
dc.relation.projectIDBQU2008-2021
dc.relation.projectID911-3 and 911-4
dc.relation.projectIDID15B
dc.rights.accessRightsrestricted access
dc.subject.cdu548
dc.subject.ucmCristalografía (Geología)
dc.titleThermotropic Liquid Crystal Developable Domains in This and Similar Systems
dc.typejournal article
dc.volume.number15
dspace.entity.typePublication
relation.isAuthorOfPublication2abd5041-98dc-440a-85bd-2e5172f03cd6
relation.isAuthorOfPublicatione8889f99-6c40-4a0d-a11b-d305a8a9ecea
relation.isAuthorOfPublication.latestForDiscoverye8889f99-6c40-4a0d-a11b-d305a8a9ecea

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