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Christophe Baravian

Researcher at University of Lorraine

Publications -  54
Citations -  1988

Christophe Baravian is an academic researcher from University of Lorraine. The author has contributed to research in topics: Rheology & Particle. The author has an hindex of 24, co-authored 54 publications receiving 1840 citations. Previous affiliations of Christophe Baravian include Centre national de la recherche scientifique & Nancy-Université.

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Liquid–crystalline aqueous clay suspensions

TL;DR: Small-angle x-ray scattering measurements of gel samples reveal strong positional and orientational orders of the particles, proving unambiguously the nematic character of the gel and, thus, clearly refuting the still prevalent “house of cards” model.
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Phase Diagrams of Wyoming Na-Montmorillonite Clay. Influence of Particle Anisotropy

TL;DR: Interacting clay particles are amenable to generate, at rest and/or under shear, large anisotropic particle associations that are not directly related to an isotropic/nematic transition of individual clay particles.
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Aqueous Suspensions of Natural Swelling Clay Minerals. 1. Structure and Electrostatic Interactions

TL;DR: An overview of the organization of colloidal charged clay particles in aqueous suspension is presented by studying different natural samples with different structural charges and charge locations through a detailed investigation of the structure factors of the various clay samples.
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Aqueous suspensions of natural swelling clay minerals. 2. Rheological characterization.

TL;DR: A comprehensive investigation of the viscoelastic behavior of different natural colloidal clay minerals in aqueous solution was reported, pointing out that in the high shear limit the suspension viscosity is still closely related to electrostatic interactions and follows the same trends as the vis coelastic properties.
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Electric-field-induced perfect anti-nematic order in isotropic aqueous suspensions of a natural beidellite clay.

TL;DR: The excess polarizability of the isotropic regions of biphasic nematic/isotropic samples is proposed to be due to pretransitional fluctuations of the spontaneous nematic order S(N) of the colloidal suspension and/or formation of chains of particles, with antinematic order of the beidellite disks in the chains.