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Drag coefficient for irregularly shaped grains: rotational dependence at various Reynolds numbers

Published online by Cambridge University Press:  13 September 2024

Álvaro Vergara
Affiliation:
Institute of Geomechanics and Underground Technology, Faculty of Civil Engineering, RWTH Aachen University, 52074 Aachen, Germany
Deheng Wei*
Affiliation:
Institute of Geomechanics and Underground Technology, Faculty of Civil Engineering, RWTH Aachen University, 52074 Aachen, Germany Key Laboratory of Ministry of Education on Safe Mining of Deep Mines, School of Resources and Civil Engineering, Northeastern University, Shenyang 110819, PR China School of Civil Engineering, The University of Sydney, NSW 2006, Australia
Raúl Fuentes
Affiliation:
Institute of Geomechanics and Underground Technology, Faculty of Civil Engineering, RWTH Aachen University, 52074 Aachen, Germany
*
Email addresses for correspondence: wei@gut.rwth-aachen.de, dwei3017@uni.sydney.edu.au

Abstract

The nature and behaviour of the drag coefficient $C_D$ of irregularly shaped grains within a wide range of Reynolds numbers $Re$ is discussed. The morphology of the grains is controlled by their fractal description, and they differ in shape. Using computational fluid dynamics tools, the characteristics of the boundary layer at high $Re$ has been determined by applying the Reynolds-averaged Navier–Stokes turbulence model. Both grid resolution and mesh size dependence are validated with well-reported previous experimental results applied in flow around isolated smooth spheres. The drag coefficient for irregularly shaped grains is shown to be higher than that for spherical shapes, also showing a strong drop in its value at high $Re$. This drag crisis is reported at lower $Re$ compared to the smooth sphere, but higher critical $C_D$, demonstrating that the morphology of the particle accelerates this crisis. Furthermore, the dependence of $C_D$ on $Re$ in this type of geometry can be represented qualitatively by four defined zones: subcritical, critical, supercritical and transcritical. The orientational dependence for both particles with respect to the fluid flow is analysed, where our findings show an interesting oscillatory behaviour of $C_D$ as a function of the angle of incidence, fitting the results to a sine-squared interpolation, predicted for particles within the Stokes laminar regime ($Re\ll 1$) and for elongated/flattened spheroids up to $Re=2000$. A statistical analysis shows that this system satisfies a Weibullian behaviour of the drag coefficient when random azimuthal and polar rotation angles are considered.

Information

Type
JFM Papers
Creative Commons
Creative Common License - CCCreative Common License - BYCreative Common License - NCCreative Common License - ND
This is an Open Access article, distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivatives licence (http://creativecommons.org/licenses/by-nc-nd/4.0), which permits non-commercial re-use, distribution, and reproduction in any medium, provided that no alterations are made and the original article is properly cited. The written permission of Cambridge University Press must be obtained prior to any commercial use and/or adaptation of the article.
Copyright
© The Author(s), 2024. Published by Cambridge University Press.
Figure 0

Figure 1. Geometry of irregularly shaped particles used in the study of the drag coefficient. (a) Grain with fractal dimension $D_f=2.287$, typically frequent for Leighton Buzzard sand. (b) Grain with fractal dimension $D_f=2.420$, frequent for highly decomposed granite.

Figure 1

Table 1. Particle shape descriptors of Leighton Buzzard sand and highly decomposed granite, based on the definitions presented in Angelidakis, Nadimi & Utili (2022) and Michaelides & Feng (2023). The flatness is herein defined as the ratio between the lengths of the major and intermediate axes; the elongation is defined as the ratio between the lengths of the intermediate and minor axes; the compactness is defined as the ratio of the area of the particle to the square of its maximum perimeter; and the sphericity is defined as the ratio of the surface area of the sphere with equivalent volume to the actual surface area of the particle.

Figure 2

Figure 2. (a) Computational domain used in the numerical study, whose dimensions make it possible to avoid the influence of the fluid–wall interaction on the fluid–particle interaction (not to scale). (b) Unstructured mesh applied in conjunction with inflation methods to optimise turbulence capture in the boundary layer. (c) Azimuthal rotation $\alpha$ anticlockwise with respect to the $z$-axis ($x$$y$ meridional plane). (d) Polar rotation $\beta$ anticlockwise with respect to the $y$-axis ($x$$z$ meridional plane).

Figure 3

Figure 3. (a) Drag coefficient $C_D$ as a function of the Reynolds number $Re$ for an isolated smooth sphere. The solid black line represents the fitted experimental values for the smooth sphere (Turton & Levenspiel 1986). The circles represent each numerical simulation. The red dashed line corresponds to the mesh resolution, showing a dependence on $Re$. (b) Percentage difference between experimental data and numerical results (in triangles).

Figure 4

Figure 4. (a) Drag coefficient $C_D$ as a function of the Reynolds number $Re$ for the LBS and HDG grains. The black solid line represents the values for the smooth sphere. The markers represent the different simulations performed. The coloured symbols shows the range of values of the azimuthal rotation $\alpha$. (b) Drag coefficient $C_D$ as a function of the Reynolds number $Re$ in the drag crisis.

Figure 5

Figure 5. (a) Drag coefficient $C_D$ as a function of the angle of incidence of the flow $\alpha$ at different $Re$ for the LBS and HDG grains. (b) Normalised projected area $A_P/ {\rm \pi}r_{d}^2$ as a function of the rotation angle of incidence $\alpha$ (with $\beta =0$) for both particles. (c) Normalised drag coefficient $C_D^*$ as a function of the angle of incidence of the flow $\alpha$ at different $Re$. The solid line represents the sine-squared function. (d) Drag coefficient $C_D$ as a function of the normalised projected area $A_P {\rm \pi}r_{d}^2$, at various Reynolds numbers $Re$. The inset shows these values for HDG grains.

Figure 6

Figure 6. Weibull probability density distributions of the drag coefficient for different random angles of incidence ($\alpha \neq \beta \neq 0$): (a) $Re=1$, (b) $Re=100$, (c) $Re=1000$, (d) $Re=10\,000$, for the LBS grain; (e) $Re=10\,000$ for the HDG grain. (f) Plot of $\ln [\ln (1/P_S)]$ versus $\ln (C_D/C_{D,0})$, where $P_S$ is the survival probability distribution.

Figure 7

Figure 7. Turbulence patterns of (a,b) the sphere, (c,d) the LBS particle, and (e,f) the HDG particle, for $Re=100\,000$. Here, (a,c,e) represent the vortex isosurfaces around the sphere and the irregular particles, and (b,d,f) are the velocity fields on a meridional plane.

Figure 8

Figure 8. Pressure profiles on the front surface of the flow for (a) the LBS particle, and (c) the HDG particle. Shear profiles on the front surface of the flow for (b) the LBS particle, and (d) the HDG particle. The figures correspond to turbulent flow in the critical regime $Re=100\,000$.