Liquid-crystalline ferroferric oxide nanocomposites: self-assembly and magnetorheological effects
Abstract
Magnetorheological (MR) fluids are a class of smart materials whose yield stress increases considerably when an external magnetic field is applied. The MR effect and sedimentation stability are two major factors for good MR fluids. In order to synthesize novel MR materials with high yield stress and enhanced sedimentation stability, a series of liquid-crystalline (LC) ferroferric oxide nanocomposites (Fe3O4@PILCs) with a core–shell structure were self-assembled by magnetic Fe3O4 nanoparticles, polyethylenimine and a cholesteryl-based LC material bearing sulfonic and carboxylic acid groups. The chemical structure, surface morphology, magnetic performance, thermal properties, and liquid-crystalline behavior of the Fe3O4@PILCs were characterized by various equipment and instruments. The MR effect, magnetic field response, and sedimentation stability of the Fe3O4@PILC-based MR fluids were investigated by various technical methods. The Fe3O4@PILC nanocomposites showed a smectic A LC phase when they were measured by the heating and cooling cycles. The MR fluids fabricated using the Fe3O4@PILC nanocomposites as suspended particles and silicone oil as a carrier liquid showed Bingham flow characteristics when an external magnetic field was applied on them, and it exhibited a maximum MR efficiency of 90 under 128 kA m−1 magnetic field strength. The enhanced MR effect of the Fe3O4@PILC-based fluids was derived from a synergistic effect between the LC orientation and the Fe3O4 particle rearrangement along the magnetic field direction. In comparison with pristine Fe3O4-based fluids, the Fe3O4@PILC-based MR fluids showed excellent sedimentation stability, which is attributed to the surface modification of Fe3O4 particles reducing the density, the sulfonic and carboxylic acid groups acting as surfactants and stabilizers, and the excellent compatibility between the organic polymer shell structure and silicone oil preventing the Fe3O4 core from settling.