research

The electrorheology of suspensions consisting of Na-Fluorohectorite synthetic clay particles in silicon oil

Abstract

Under application of an electric field greater than a triggering electric field Ec0.4E_c \sim 0.4 kV/mm, suspensions obtained by dispersing particles of the synthetic clay fluoro-hectorite in a silicon oil, aggregate into chain- and/or column-like structures parallel to the applied electric field. This micro-structuring results in a transition in the suspensions' rheological behavior, from a Newtonian-like behavior to a shear-thinning rheology with a significant yield stress. This behavior is studied as a function of particle volume fraction and strength of the applied electric field, EE. The steady shear flow curves are observed to scale onto a master curve with respect to EE, in a manner similar to what was recently found for suspensions of laponite clay [42]. In the case of Na-fluorohectorite, the corresponding dynamic yield stress is demonstrated to scale with respect to EE as a power law with an exponent α1.93\alpha \sim 1.93, while the static yield stress inferred from constant shear stress tests exhibits a similar behavior with α1.58\alpha \sim 1.58. The suspensions are also studied in the framework of thixotropic fluids: the bifurcation in the rheology behavior when letting the system flow and evolve under a constant applied shear stress is characterized, and a bifurcation yield stress, estimated as the applied shear stress at which viscosity bifurcation occurs, is measured to scale as EαE^\alpha with α0.5\alpha \sim 0.5 to 0.6. All measured yield stresses increase with the particle fraction Φ\Phi of the suspension. For the static yield stress, a scaling law Φβ\Phi^\beta, with β=0.54\beta = 0.54, is found. The results are found to be reasonably consistent with each other. Their similarities with-, and discrepancies to- results obtained on laponite-oil suspensions are discussed

    Similar works

    Full text

    thumbnail-image

    Available Versions

    Last time updated on 12/11/2016
    Last time updated on 05/06/2019