Year-end Sale % OFF 
Abstract
Monodisperse sols of β-FeOOH crystals are used for the detection and structural analysis of vortices formed prior to the transition of laminar into turbulent flow, the experimental tools used being both characteristic qualitative periodicities observed in flow light scattering and quantitative variations in its intensity as a function of shear rate. The proportionality between viscosity and initial shear rate, expressed in the classical equation of Taylor, is taken advantage of for the determination of viscosities in dilute dispersed systems using discontinuities in flow light scattering at the critical shear rate as a very sensitive argument which is under certain circumstances applicable also to dispersions of spherical particles.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
