The Isotropic-Nematic Interface in Suspensions of Na-Fluorohectorite Synthetic Clay

Autor: Yves Méheust, M. Engelsberg, Kenneth D. Knudsen, Nils I. Ringdal, Henrik Hemmen, Jon Otto Fossum, Eduardo N. de Azevedo, Elisabeth Lindbo Hansen
Přispěvatelé: Géosciences Rennes (GR), Université de Rennes 1 (UR1), Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre Armoricain de Recherches en Environnement-Centre National de la Recherche Scientifique (CNRS), Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre Armoricain de Recherches en Environnement-Centre National de la Recherche Scientifique (CNRS)
Jazyk: angličtina
Rok vydání: 2009
Předmět:
Zdroj: Langmuir
Langmuir, American Chemical Society, 2009, 25 (21), pp.12507-12515. ⟨10.1021/la901784k⟩
Langmuir, 2009, 25 (21), pp.12507-12515. ⟨10.1021/la901784k⟩
ISSN: 0743-7463
1520-5827
DOI: 10.1021/la901784k⟩
Popis: International audience; Colloidal suspensions of Na-fluorohectorite synthetic clay platelets in saline water exhibit coexisting isotropic andnematic phases, due to gravitational separation of the polydisperse particles. Westudy the ordering of the platelets at the interfaces between various coexisting phases. Four different experimental techniques are employed: visual observation of birefringence, synchrotron wide angle and small-angle X-ray scattering, and magnetic resonance imaging. We find that at the narrow isotropic sol-nematic sol interface the platelets are lying horizontally, i.e. with their mean platelet normal along the vertical direction. The experiments indicate that the platelets align homeotropically both at the isotropic sol-nematic sol interface and at the nematic sol-wall interface. We further investigate the complex alignment effect of a horizontally applied magnetic field in the nematic sol, and we compare it with the adjacent nematic gel.
Databáze: OpenAIRE