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Experimental and numerical study of rigid particles with two planes of symmetry approaching a stable, stationary orientation while sedimenting

Published online by Cambridge University Press:  27 April 2026

Chandra Shekhar
Affiliation:
Institute of Fundamental Technological Research, Polish Academy of Sciences, ul. Pawińskiego 5B, Warsaw 02-106, Poland
Harish N. Mirajkar
Affiliation:
Institute of Fundamental Technological Research, Polish Academy of Sciences, ul. Pawińskiego 5B, Warsaw 02-106, Poland
Piotr Zdybel
Affiliation:
Institute of Fundamental Technological Research, Polish Academy of Sciences, ul. Pawińskiego 5B, Warsaw 02-106, Poland
Yevgen Melikhov
Affiliation:
Institute of Fundamental Technological Research, Polish Academy of Sciences, ul. Pawińskiego 5B, Warsaw 02-106, Poland
Maria L. Ekiel-Jeżewska*
Affiliation:
Institute of Fundamental Technological Research, Polish Academy of Sciences, ul. Pawińskiego 5B, Warsaw 02-106, Poland
*
Corresponding author: Maria L. Ekiel-Jeżewska, mekiel@ippt.pan.pl

Abstract

This work investigates experimentally and numerically the dynamics of rigid particles with two orthogonal symmetry planes settling under gravity in a highly viscous fluid at a Reynolds number much smaller than one. Joshi & Govindarajan (2025 Phys. Rev. Lett. 134(1), 014002), showed theoretically that for such shapes, the dynamics are qualitatively different for different signs of the product of two rotational–translational mobility coefficients, evaluated with respect to the particle centre of mass in a symmetric reference frame. However, upon examining a particle’s shape, it is not immediately evident if this product is negative, positive or zero. In this paper, we demonstrate how to estimate these coefficients and the sign of their product from experiments, using special initial orientations, and also numerically, based on the Stokes equations. Especially interesting are the ‘settlers’ – such particles that reorient and approach a stationary stable orientation, and we focus our study on this class of shapes. We show experimentally that cones, crescent moons, arrowheads and open flat rings are the settlers, and we evaluate from the experiments their rotational–translational mobility coefficients. Then, we reconstruct each experimental shape as a rigid conglomerate of many touching beads, and use the precise Hydromultipole code to calculate the mobility coefficients for the conglomerate. The numerical and experimental values are close enough to determine that the particles are the settlers, and to estimate the characteristic reorientation time scales. Our findings apply to non-Brownian micro-objects in water-based solutions – experimentally by the similarity principle and theoretically based on the Stokes equations. The reorientation of sedimenting rigid particles to a stationary stable configuration in a relatively short time might be used for environmental, biological, medical or industrial applications.

Information

Type
JFM Papers
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2026. Published by Cambridge University Press
Figure 0

Figure 1. Two special motions of a particle with $x\rightarrow -x$ and $y\rightarrow -y$ symmetries are illustrated: (a) case A, rotation of the particle around $y=Y$; (b) case B, rotation of the particle around $x=X$. Here $xyz$ is the coordinate system moving with the particle, shown in (c), $XYZ$ is the laboratory frame of reference and $\theta$ is the angle between the $z$ and $Z$ axes.

Figure 1

Figure 2. Schematic representation of the experimental set-up.

Figure 2

Figure 3. The objects used in the experimental studies, shown from different perspectives, with their dimensions indicated in millimetres. The scale bar (white line) represents 5 mm.

Figure 3

Table 1. Physical properties of the various objects used during the experimental study.

Figure 4

Table 2. The number of experimental trials performed for the indicated initial orientations of the objects, along with the number of trials selected for quantitative analysis of the reorientation. Names of the objects: C, cone; A, arrowhead; M, crescent moon; R$i$, ring with the opening width equal to $i = 1, 2, 3, 4$ mm. For the crescent moon, the numbers without and with an asterisk refer to the trials with non-prewetted and prewetted particles, used to compute $\mu _{42}$ and $\mu _{51}$, respectively.

Figure 5

Figure 4. Snapshots from three experimental trials showing time-dependent position and orientation of a single sedimenting object: (a) cone, (b) arrowhead and (c) crescent moon. The images were recorded simultaneously by two cameras (top and bottom halves of each panel). Gravity points leftwards, and the particles move from right to left.

Figure 6

Figure 5. Snapshots from four experimental trials showing time-dependent position and orientation of a single sedimenting ring with the opening of (a) 1 mm, (b) 2 mm, (c) 3 mm, (d) 4 mm. The images were recorded simultaneously by camera 1 (top half of each panel) and camera 2 (bottom half of each panel). Gravity points leftwards, and the particles move from right to left.

Figure 7

Figure 6. Vertical component $U_Z$ of the sedimentation velocity of the object’s centre for the experimental trials shown in figures 4 and 5. Names of the objects: C, cone; A, arrowhead; M, crescent moon; R$i$, ring with the opening width equal to $i = 1, 2, 3, 4$ mm.

Figure 8

Figure 7. Reorientation of particles of different shapes in the experimental trials shown in figures 4 and 5. The time dependence of $\tan (\theta /2)$ for the experimental data (symbols) is approximated (solid lines) by the exponential function (4.1) with the fitted values of the parameters $A$ and $\tilde {\tau }$, listed in Appendix C. Names of the objects: C, cone; A, arrowhead; M, crescent moon; R$i$, ring with the opening width equal to $i = 1, 2, 3, 4$ mm. The plots for different objects are shifted in time to reach $\tan (\theta /2)=1$ at the same time instant.

Figure 9

Figure 8. Snapshots from the experimental trials showing time-dependent position and orientation of a single sedimenting prewetted crescent moon initially at the inverted orientation. The images were recorded simultaneously by two cameras (top and bottom half of each panel). Gravity points leftwards, and the particles move from right to left.

Figure 10

Figure 9. Snapshots from two experimental trials with the inclined initial orientation, showing time-dependent position and orientation of a single sedimenting object: (a) arrowhead, (b) ring with the opening of 1 mm. The images were recorded simultaneously by two cameras (top and bottom half of each panel). Gravity points leftwards, and the particles move from right to left.

Figure 11

Table 3. The average parameters: particle velocity $U_{\!f}$ in the stationary configuration, coefficients $1/\tilde {\tau }_{51}$ or $1/\tilde {\tau }_{42}$, and the dimensionless mobility coefficients based on the centre of mass as the reference point. Particle types: C, cone; A, arrowhead; M, crescent moon, R$i$, ring with the opening width equal to $i = 1, 2, 3, 4$ mm.

Figure 12

Table 4. The Reynolds, Re, Stokes, St,and Archimedes, Ar, numbers in our experiments are much smaller than one.

Figure 13

Figure 10. Shapes of the cone, arrowhead and open rings used in the experiments, represented as conglomerates of $N$ touching identical spherical beads. The particles are shown in their stationary stable configuration at $\theta =0$, with $H$ along gravity. (a) Cone, $N=6189$; (b) arrowhead, $N=4896$; (c) open ring with a 1 mm wide gap, $N=5182$; (d) open ring with a 3 mm wide gap, $N=5110$.

Figure 14

Figure 11. Shape of the crescent moon represented as a conglomerate of $N$ touching identical spherical beads. The figure shows three auxiliary surface meshes delimiting the boundary of the modelled body (see Appendix D.4). The crescent moon is shown in its stationary stable configuration at $\theta =0$, with $H$ along gravity. (a) Crescent moon, $N=5513$; (b) crescent moon, front and side views.

Figure 15

Table 5. The dimensionless mobility coefficients based on the centre of mass as the reference point, as defined in (2.4), evaluated from the bead model of the particles used in our experiments.

Figure 16

Table 6. Percentage difference between experimental (table 3) and simulated (table 5) values for mobility coefficients $\mu _{33}$, $\mu _{42}$ and $\mu _{51}$, calculated as $\Delta \mu = (\mu ^{{exp}} - \mu ^{{sim}}) / \mu ^{{exp}}$.

Figure 17

Figure 12. Parametric study of aperture-controlled ring fragments. (a) Geometry and notation. (bd) Mobilities as a function of $\Delta \vartheta$: (b) $\mu _{33} \,({R}/{L})$, (c) $\mu _{42}\,( {R}/{L})^2$ and (d) $\mu _{51} \,({R}/{L})^2$. Blue dashed curves, circular rings; orange dashed curves, elliptical rings ($a/b\approx 1.43$). Red stars (R1–R4) are the numerical values for rings with opening widths $=1,2,3,$ and $4$ mm taken from table 5.

Figure 18

Figure 13. Stationary stable orientations of different objects, corresponding to $\theta =0$. The shapes and their orientation are taken from the experimental images.

Figure 19

Figure 14. Snapshots from three experimental trials, demonstrating 3-D reorientation of a single sedimenting object: (a) crescent moon in the inverted initial orientation, (b) ring with the opening of 1 mm in the inverted initial orientation and (c) ring with the opening of 4 mm in the inclined initial orientation. The images were recorded simultaneously by two cameras (top and bottom half of each panel). Gravity points leftwards, and the particles move from right to left.

Figure 20

Figure 15. A schematic binary image with the computed equivalent ellipse and the indicated inclination angle $\alpha$. The ellipse is centred at the object’s centroid, and its principal axes are also marked.

Figure 21

Table 7. The fitting parameters $A$ and $1/\tilde {\tau }$ of the exponential decay fit (4.1) to the data from seven exemplary experimental trials plotted in figure 7 for various shapes, together with the coefficient of determination $R^2$ that shows the goodness of the fit.

Figure 22

Figure 16. The surface meshes used in the construction of the bead model for the crescent moon.

Figure 23

Table 8. Convergence analysis of the bead model. The coefficients $\mu$ are compared between the highest resolution model used in this work (fine) and the preceding discretisation step (coarse). Resolution is denoted by the number of beads $N$ and the discretisation parameter length $L/d$. The relative difference $\Delta \mu$ is calculated as $(\mu ^{\textit{fine}} \! - \!\mu ^{\textit{coarse}}) / \mu ^{\textit{fine}}$.