[Complex suspension rheological behavior in the range of flow geometry]
By
Table of Contents
ABSTRACT5
INTRODUCTION6
LITERATURE REVIEW13
Importance of Rheology13
Colloidal Systems13
Definition and Classification13
Suspensions14
Foam14
Emulsions15
Forces acting on colloidal systems15
Rheological Properties of Kaolin Suspensions15
Factors affecting Kaolin Suspension Rheology15
Surface Charges and Structure of Kaolin Suspension16
Classifications of Fluid Behavior19
Newtonian Fluid20
Non-Newtonian Fluid20
Times-Independent Behaviour of Fluid21
Shear thinning fluids22
Shear-thickening fluid behavior23
Viscoplastic fluid behavior23
Time-dependent Behaviour of Fluid24
Thixotropy25
Rheopexy26
The DLVO Forces27
The Van der Waals Attractive Force27
The Electrostatic Force28
The Non-DLVO Forces28
Bridging Interactions28
Steric Repulsions29
Rheological Instruments30
Concentric Cylinder Rheometer30
Four-bladed Vane Rheometer32
Problems encountered on Concentric Cylinder Rheometer34
Viscous Heating34
Slip or Wall effects34
Cavitation35
Secondary Flow36
EXPERIMENTAL METHOD37
Rheological properties of a fluid38
Constitutive38
Main types of behaviour40
Fluid threshold41
Macroscopic properties and rheological Suspension42
Newtonian Suspensions42
Methodology of homogenization42
The representation of VER step43
The location step43
The homogenization step43
Method Estimation44
Elastic modulus vs. yield stress45
Yield stress46
Simplified modelling of the liquid-solid transition46
Micromechanical modelling of the transition in liquids and solids50
Experimental study of the structure and destructing of a thixotropic material54
RESULTS AND DISCUSSION56
CONCLUSION AND FUTURE WORK65
Scope of the Studies72
APPENDIX77
Abstract
It has been reviewed in this study that fluid mechanics and rheology of dense suspensions, emphasizing investigations of microstructure and total stress. “Dense” or “highly concentrated” suspensions are those in which the average particle separation distance is less than the particle radius. For these suspensions, multiple-body interactions as well as two-body lubrication play a significant role and the rheology is non-Newtonian. We also include investigations of multimodal suspensions, but not those of suspensions with dominant non-hydrodynamic interactions. It was considered results from both physical experiments and computer simulations and explore scaling theories and the development of constitutive equations. The study has also developed an approach for scaling to study the behaviour of a macroscopic particle composite material. To this end, we presented the main characteristics of homogenization methods to obtain a characterization of the equivalent homogeneous behaviour of a heterogeneous material. We also noted the main results obtained by the homogenization approach for nonlinear isotropic particle suspensions in non-deformable fluid-Hershel Bulkley. We then studied the effect of particle poly-dispersity on the values rheological parameters of a bi-disperse suspension. These results also show that the structure to assess and disintegration of a suspension of colloidal particles in a non- thixotropic colloidal fluid, it suffices to study the properties of the suspending fluid. From this result, it is necessary to perform further experiments not only on the carrier fluid, but also in the presence of non-colloidal particles order to have accurate results. Our preliminary results show that this line of study is very promising.
Introduction
Kaolin is said to be an industrial mineral that possesses many distinct physical and chemical properties making it very useful in different industrial applications such as in paper industry. Kaolin is used in adding rigidity and strength to rubber products as well. It is also added to plastics, ceramics and paints wherein it gives smoother surface, chemical resistance and desirable flow properties (Murray and Kogel, 2005). All this variety of properties is achieved at low cost of kaolin.
This study aims to come-up with useful results of rheological behaviour specifically of non-Newtonian flow, since there is an insufficient data available to predict the flow behaviour of these ...