Diluted suspensions (packing fraction Φ<2%) can for many purposes be treated as Newtonian fluids with a relative viscosity μsusp=μfluid(1+2.5Φ+O(Φ2))
(A. Einstein, Ann. d. Phys. 19, 289 (1906) and 34, 591 (1911))
However, the multitude of equations for the relative viscosity in the high packing fraction regime poses the question if a concentrated suspension is still well characterized as a fluid. To test this, we studied the linear instability of the interface between a concentrated suspension and clear water and compared it to the well studied Rayleigh Taylor instability which takes place, when a more dense fluid is stratified on top of a less dense fluid.
The experiments are performed in a closed Hele Shaw cell of 16 x 8 x 0.4 cm. By turning the cell around a horizontal axis an initially sedimented layer of glass beads forms a layer of concentrated suspension on top of pure water.


After tracking down the suspension-water interface we do a Fourier decomposition. Then the temporal evolution of each Fourier mode is tried to fit with an exponential growth law as shown in Figure 3.
The average growth rate of these fits as a function of the wavenumber of the corresponding Fourier mode is plotted in Figure 4. This dispersion relation can then be compared to the theoretical predictions of a 2 fluid model.


The interface of a concentrated suspension stratified over the pure fluid shows a density driven instability. A comparison of the measured dispersion relation with the theoretical results for a 2 fluids model indicates that concentrated suspensions show still fluidlike behaviour. More work is needed as neither the viscosity nor the density of the suspension were measured in the experiment so that these variables were fit parameters in the comparison with the theory.
![]() Andreas Engel Universität Oldenburg |
![]() Adrian Lange MPI, Dresden |
![]() Ingo Rehberg Universität Bayreuth |
![]() Michael Scherer |
![]() Camilla Völtz |