Hydrodynamics of inhomogeneous agglomerates for a fractal dimension of 2.5 at intermediate Reynolds numbers: Effect of agglomerate sizes and Reynolds numbers

In this study, the effect of agglomerate sizes for a fractal dimension (D-f) of 2.5 on the hydrodynamics at intermediate Reynolds numbers (Re) of 1-120 was assessed. The results show that a core behaves like a solid sphere that exists in the central region inside the agglomerate. In addition, increasing the agglomerate diameter represents adding an extra permeable layer outside the agglomerate. For a larger Re or a smaller agglomerate diameter, the fluid can enter and penetrate through the agglomerate more easily, and the hydrodynamic characteristics of agglomerates deviate more from those of solid spheres. The effect of diameters on the velocity and pressure profiles becomes less significant with the increase in the diameter. Based on the simulated results, the drag ratio has an approximately linear relationship with Re, and its intercept has an exponential relationship with the dimensionless agglomerate diameter. Compared with homogeneous porous spheres, the drag ratio of the agglomerate is different. The effect of diameters on the drag ratio decreases as the diameter increases. It should be noted that the effect of radially varying permeability on inhomogeneous agglomerates should not be ignored and that the effect weakens as Re increases.

Automated summary

This study assessed the effect of agglomerate sizes with a fractal dimension (D-f) of 2.5 on hydrodynamics at intermediate Reynolds numbers (Re) of 1-120. The findings indicate that the core of the agglomerate behaves like a solid sphere located in the central region. Increasing the agglomerate diameter adds a permeable layer outside the agglomerate. The fluid can easily enter and penetrate through smaller agglomerates or at higher Re, leading to greater deviation from the characteristics of solid spheres.