Open Access Article
Carolina
van Baalen
a,
Laura
Alvarez
b,
Robert W.
Style
a and
Lucio
Isa
*a
aLaboratory for Soft Materials and Interfaces, Department of Materials, ETH Zürich, Vladimir-Prelog-Weg 5, 8093 Zürich, Switzerland. E-mail: lucio.isa@mat.ethz.ch
bUniv. Bordeaux, CNRS, CRPP, UMR 5031, F-33600 Pessac, France. E-mail: laura.alvarez-frances@u-bordeaux.fr
First published on 1st April 2025
Active systems comprising micron-sized self-propelling units, also termed microswimmers, are promising candidates for the bottom-up assembly of small structures and reconfigurable materials. Here we leverage field-driven colloidal assembly to induce structural transformations in dense layers of microswimmers driven by an alternating current (AC) electric field and confined in a microfabricated trap under the influence of gravity. By varying the electric field frequency, we realize significant structural transformations, from a gas-like state at high frequencies to dynamically rearranging dense crystalline clusters at lower frequencies, characterized by vorticity in their dynamics. We demonstrate the ability to switch between these states on-demand, showing that the clustering mechanism differs from motility-induced phase separation. Our results offer a valuable framework for designing high-density active matter systems with controllable structural properties, envisioned to advance the development of artificial materials with self-healing and reconfiguration capabilities.
Microscopic active systems can display non-trivial density profiles and critical fluctuations, even at densities much lower than the bulk jamming density found in passive systems. In such systems, the self-propelling units, often referred to as microswimmers or active particles, may undergo dynamic clustering akin to a liquid–gas phase separation4–10 or crystallization11–17 at relatively low particle densities and in the absence of any temperature changes or attractive inter-particle interactions, making microswimmers promising candidates for the bottom-up assembly of small structures and reconfigurable materials that can change their properties on demand.
Numerical studies have shown that microswimmer self-assembly can arise through self-trapping driven by the interplay of out-of-equilibrium collisions and finite reorientation times. This mechanism is fundamentally governed by microswimmer density, self-propulsion velocity, and rotational diffusion.7,8,18 Although attractive inter-particle interactions are not required, they can facilitate the onset of collective motion and expand the range of dynamic structures achievable.7,19,20 Indeed, different experiments have demonstrated the existence of various collective states of synthetic microswimmers, including polar liquid states,21,22 turbulence,23 swarms,24 and living crystals.15,17 Nonetheless, experimentally achieving a wide range of on demand controlled structures remains a challenging task, in particular, due to the need for a single experimental system with controlled microswimmer densities, as well as in situ control over the microswimmers' self-propulsion speed and interaction potential.
In this manuscript, we utilize gravity and electric field-driven colloidal assembly to achieve controlled structural organization and self-propulsion dynamics in dense layers of colloidal microswimmers. By varying the frequency of the applied electric field, we induce structural transitions spanning gas-like states to self-assembled motile crystallites, accompanied by emergent vorticity at lower field frequencies. Furthermore, we demonstrate the ability to switch between these states on demand by modulating the field frequency. This approach enables the creation of a high-density active matter system with strong, tunable interactions, distinct from prior studies emphasizing assembly driven primarily by motion persistence.15,17
We allow the active system to evolve for 9 min under a fixed applied peak-to-peak voltage of Vpp = 4 V (corresponding to a field strength of
) and varying frequency from f = 800 Hz to f = 200 Hz (Videos S1–S4, ESI†). It is worth noting that the chamber boundaries exhibit strong repulsion upon activation of the AC field, driven by outward hydrodynamic flows. These flows arise from electric field gradients at the interface of the electrode and the chamber material printed on it, resulting from their differing electrical properties.29 Therefore particles do not enter a region of approximately 30 μm from the walls of the chamber, hence they cannot escape through the top hole over the course of the experiment, and the chamber thus effectively acts as a trap. As shown qualitatively in Fig. 1e–h, applying different electric field frequencies results in markedly distinct structural features of the active colloidal monolayers. At a frequency of f = 800 Hz, the microswimmers explore the entire space of the trap, with an average probability density P(ρ) as a function of height z that decays gradually from the bottom of the trap to the top (Fig. 1i). At f = 500 Hz, the structure of the microswimmers' monolayer appears similar, but with a higher particle density at the bottom of the trap. Decreasing the frequency further to f = 300 Hz results in increasing particle densities at the bottom, and finally at f = 200 Hz only a dense sediment is left at the bottom of the trap, while no free swimming particles remain in the top part, as quantitatively apparent from the sharp drop in P(ρ) versus z. To understand if the changing structure of the monolayers can be a result of changes in the self-propulsion velocities of the microswimmers, we measure their free swimming velocities in the absence of gravity, i.e. above a horizontal substrate (i.e. α = 0°), as shown in Fig. 1j. Upon decreasing the frequency of the electric field from f = 800 Hz to f = 500 Hz, the mean self-propulsion velocities of the microswimmers remain approximately constant at around v ≈ 20 μm s−1. However, further reducing the frequency from f = 500 Hz to f = 200 Hz, causes a marked decline in the mean self-propulsion velocity to v ≈ 7 μm s−1. The sedimentation force acting on a single microswimmer, as approximated from the buoyant weight of a 3 μm SiO2 sphere, is Fg ≈ 0.22 pN in our experiment. In contrast, the observed self-propulsion velocities at frequencies f = 800, 500 and 300 Hz correspond to active forces, obtained from Stokes' drag, of Fs ≈ 0.51, 0.49, and 0.37 pN, respectively. Thus, at these frequencies, the average self-propulsion force is sufficient to enable microswimmers to overcome gravitational forces and swim upwards. A minor effect of gravity becomes discernible at these frequencies, as evidenced in the polar plot in Fig. 1k. Here, we show the mean instantaneous velocities measured in the top part of the trap (i.e., at α = 45°) as a function of the swimming direction for f = 800, 500 and 300 Hz, revealing self-propulsion velocities approximately ∼3 μm s−1 higher in the downward direction compared to the upward direction. Conversely, at f = 200 Hz, the average self-propulsion force of the microswimmers falls below the threshold needed to swim upwards (Fs ≈ 0.18 pN), which explains the absence of microswimmers in the top part of the trap at this frequency. The pronounced changes in the suspension microstructure with decreasing field frequency, however, cannot be solely attributed to variations in microswimmer persistence, as we will discuss in Sections 2.2–3.
We note that changing the applied field strength provides an additional handle to modify the structural properties of the active monolayers, as shown in Fig. 1l. Increasing the applied peak-to-peak voltage from Vpp = 2 to 5 V at a fixed frequency of f = 200 Hz slightly decreases the overall density of the sediment and yields an increasing number of voids within it. We also observe an increasing mobility of the particles within the structures upon increasing the applied peak-to-peak voltage, which is likely responsible for the less compact structure observed at Vpp = 5 V compared to Vpp = 4 V. Nevertheless, in what remains, we will focus on the effect of modulating the frequency of the electric field, which allows for a greater range of distinct structural features.
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| Fig. 2 Static structural information of microswimmer monolayers at different frequencies. (a)–(d) Snapshots of the system after 9 min of equilibration at different frequencies at Vpp = 4 V. Particles are color-coded according to their local orientation. The frame color-coding corresponds to Fig. 1e–h. (e) Correlation function of the local orientation versus distance normalized by the particle size for the different f. (f) Distribution of the absolute value of the hexagonal order parameter ψ6 (left) and typical snapshots, with particles color-coded according to the absolute value of ψ6. (g) Distribution of void sizes (left) and typical snapshots of identified voids (right). Scale bars: 50 μm. | ||
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| Fig. 3 Dynamics of microswimmer monolayers: the presence of vorticity. (a)–(d) Snapshots of the system after 9 min of equilibration at different frequencies at Vpp = 4 V, particles are color-coded according to their direction of motion extracted from the velocity vector. The arrows indicating the direction of motion in (b)–(d) show the presence of vortices. Frame colorcoding corresponds to Fig. 1a–d. (e) Probability distributions of the absolute vorticity at different frequencies (see Section 5.1 for details on the calculation). (f) Snapshot of a larger field of view corresponding to (c), color-coded according to the local vorticity values. (g) Probability distributions of the bond duration of particles at different frequencies. Note that for lower frequencies bond durations exceed the timescale of the experiment, hence the true distribution is not fully displayed. Scale bars: 50 μm. | ||
Decreasing the frequency to f = 500 Hz leads to the emergence of collective motion within the system. Specifically, Fig. 3b illustrates vortex-like dynamics at this frequency, marking a significant shift from the uncorrelated motion observed at f = 800 Hz. Similarly, at lower frequencies (f = 300 Hz, Fig. 3c, and f = 200 Hz, Fig. 3d), the crystallites in the system also exhibit vortex-like behavior, indicating the prevalence of rotational dynamics across these frequencies.
To quantify this behavior, we calculate the vorticity ω [s−1] of the microswimmers at different frequencies and analyze the probability distribution of the absolute vorticity (Fig. 3e). At f = 800 Hz, the probability distribution exhibits a sharp peak at |ω| = 0, which gradually decays to zero at approximately |ω| ≈ 0.9 s−1. Reducing the frequency to f = 500 Hz slightly decreases the peak probability at |ω| = 0 and extends the tail of the distribution. At f = 300 Hz, this extension becomes significantly more pronounced, reflecting an increase in rotational activity. Further lowering the frequency to f = 200 Hz results in the emergence of a secondary peak around |ω| ≈ 0.7 s−1, marking a substantial enhancement of rotational motion within the system.
Remarkably, the state of our system at frequencies f ≤ 300 Hz shares similarities with previous experiments involving active chiral Quincke rollers,36,37 magnetically rotating colloidal rods,38 and spinning starfish embryo crystals.11 However, unlike those systems, the active agents in our study lack intrinsic chirality or spinning behavior. The spontaneous vortical dynamics of hexagonally packed aggregates comprising randomly oriented Janus particles has been numerically predicted using a pusher-type squirmer model,39 where vorticity arises from microswimmer orientation and the geometry of the hexagonally packed aggregates. Fig. 3f shows a representative spatial map of vorticity for the low-frequency case, highlighting regions of correlated vorticity associated with crystallites rotating almost rigidly. Neighboring crystallites tend to rotate in opposite directions, as evidenced by the alternating blue and red regions in the figure. This cogwheel-like behavior likely results from hydrodynamic interactions, where a rotating crystallite's flow field drags its neighbor into phase-locked counter-rotation, as also reported in ref. 39.
To further assess the rigidity of these structures, we analyze the distribution of bond durations, defined as the duration of geometrical contact between neighboring particles, across different frequencies (Fig. 3g). At higher frequencies (f = 800 Hz and f = 500 Hz), bonds are predominantly short-lived, with the distribution falling to zero within the 1-minute measurement time frame. As the frequency decreases, the average bond duration increases markedly. At f = 300 Hz and f = 200 Hz, a significant fraction of bonds persist beyond the measurement time frame, highlighting the emergence of stable, coordinated assemblies that remain intact over extended periods.
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| Fig. 4 Condensation of microswimmers under gravity by switching the frequency of the AC electric field. (a) Snapshots of the system at different times after switching the frequency from 800 Hz to 200 Hz. Particles are color-coded according to the size of the cluster they belong to. (b) Cluster size distributions at 0, 1, 3, and 60 seconds after switching the AC field frequency from 800 Hz to 200 Hz. (c) Trajectories of clusters formed upon switching the frequency of the electric field (increasing time from blue to green). (d) Sedimentation speed of clusters as a function of their size. Error bars represent the standard deviation over at least 20 measurements. (e) High magnification snapshots of the system at different times after switching the frequency from 800 Hz to 200 Hz. Particles are color-coded according to their orientation, with the cap artificially colored. Black arrows indicate the direction of the velocity vector for each particle. See Fig. S2 (ESI†) for the corresponding raw images. (f) Probability distributions of the difference between the cap orientation and the orientation of the velocity vector 5 seconds before (blue) and 5 seconds after (mint green) switching the AC electric field. Scale bars: 50 μm. | ||
To gain a deeper understanding of the particle-level mechanisms driving cluster formation, we analyze the orientation of the microswimmer caps (Video S5, ESI†). In Fig. 4e, high-magnification images show the metallic caps of the Janus microswimmers color-coded by their orientations (θ0), with the direction of motion indicated by black arrows extracted from the velocity vector (θv). At f = 800 Hz (first panel, t = 0.0 s), interparticle interactions are minimal, and the difference between θ0 and θv is small, as seen in the black arrows that are mostly perpendicular to the caps. This is corroborated by the narrow normal distribution of θv–θ0 centered around zero (dark blue data in Fig. 4f). After switching the frequency to f = 200 Hz, we observe that the orientation of the caps and the black arrows begin to deviate from perpendicularity and particles are drawn together, regardless of their cap orientation (second panel in Fig. 4e). Consequently, the particles form clusters in which they assume random orientations, as shown in the last panel of Fig. 4e. The difference between θ0 and θv after switching to f = 200 Hz is shown by the green data in Fig. 4f. The distribution broadens to larger values, and the peak has shifted to around π/2 due to the downward sedimentation of the clustered Janus particles. Thus, the formation of motile clusters in this system appears unrelated to motion persistence or to the occurrence of collisions between the microswimmers, and instead appears to stem from attractive colloidal inter-particle interactions resulting from EHD flows around the Janus microswimmers, as discussed in more detail in Section 3.
We probe the frequency-driven changes in the nature of the fluid flows around the Janus microswimmers by adding small (2R = 200 nm) polystyrene (PS) tracer particles to the experimental system (Fig. 5). At f = 800 Hz, the Janus microswimmer moves at a relatively high self-propulsion speed, while drawing tracer particles (yellow) toward the silica hemisphere and releasing them from the metallic hemisphere. Notably, a fraction of the tracer particles accumulates near the metallic hemisphere (Fig. 5b), likely due to positive dielectrophoresis (pDEP) arising from the strong electric field gradient generated by the potential difference between the metallic hemisphere and the electrode surface.40 When the frequency is reduced to f = 200 Hz, the microswimmer slows down, and the tracer particles are attracted towards the Janus microswimmer, where they distribute around its entire circumference (Fig. 5c). This isotropic distribution indicates that contractile fluid flows towards the Janus microswimmer become more pronounced and evenly distributed as the frequency decreases.40
In prior studies, the assembly behavior of metallo-dielectric Janus microswimmers under perpendicular AC electric fields has been investigated primarily in the MHz frequency regime. These studies report the formation of self-assembled chains,24 swarms,24 and long-ranged repulsive states.24,41 Additionally, the formation of 2D networks under parallel high-frequency AC electric fields has also been observed (e.g., ref. 42 and 43). In such high-frequency AC electric fields, inter-particle interactions are predominantly governed by dipolar interactions, which arise from the differing polarization coefficients of the dielectric and metallic hemispheres of the Janus particles.
In contrast to these earlier studies, our experiments focus on the sub-kHz frequency range, where the applied frequency is several orders of magnitude lower than those typically associated with electric field-induced dipolar interactions.24,44 In this regime, particle assembly under a perpendicular AC electric field is governed by a complex interplay of frequency-dependent hydrodynamic effects.26,27,45–47 Specifically, induced-charge electroosmotic (ICEO) flows dominate in the kHz range. ICEO arises from the interaction between the applied electric field and the electric double layer (EDL) induced on the surface of the polarizable Janus particle. The characteristic timescale for this process is described by the particle charge relaxation time, τp = k−1R/D, where k−1 is the Debye length, R is the particle radius, and D is the ionic diffusion coefficient. For our experimental conditions, τp corresponds to a frequency of approximately 4.4 kHz (detailed calculations can be found in S4, ESI†). At frequencies below this threshold, the EDL on the particle has sufficient time to fully develop, enabling the nonlinear fluid flows associated with ICEO.
As the frequency decreases further into the sub-kHz range, electrohydrodynamic (EHD) flows begin to dominate near conducting surfaces, such as the bottom electrode in our experiments. The emergence of EHD flows is governed by the electrode charge relaxation time, τe = k−12h/D, where now instead of the particle radius R, the distance between the two electrodes 2h becomes the relevant length scale. For our setup, τe corresponds to a frequency of approximately 200 Hz (detailed calculations can be found in S4, ESI†). At frequencies approaching this value, the EDL at the electrode has sufficient time to fully form, creating a strong interaction with the distorted electric field near the particle. This interaction generates localized field gradients that drive fluid motion characteristic of EHD flows.
The transition from ICEO to EHD flows is evident in our experiments, where we observe a sharp decline in microswimmer self-propulsion velocity at frequencies below 500 Hz. Tracer experiments (Fig. 5a) further support this transition, showing an accumulation of tracer particles around the entire circumference of the Janus microswimmer. This behavior is driven by strong inward convective flows, which are a hallmark of EHD near conducting surfaces.40
Interestingly, we observe crystallization for bare silica spheres (i.e., without the Pd coating) across all explored frequencies (see Fig. S3, ESI†). This contrasts with the behavior of the Janus particles, highlighting the competitive roles of ICEO and EHD flows in assembly dynamics. The metallic cap of the Janus microswimmer plays a crucial role in ICEO, as the disparity in polarizability between the metallic and dielectric hemispheres enhances ICEO flows around the more polarizable metallic hemisphere. This intensified ICEO flows disrupt crystallization at higher frequencies, delaying its onset to lower frequencies. In the absence of the metallic cap, ICEO is diminished, allowing crystallization to occur even at higher frequencies. These observations are consistent with our experimental findings and underscore the intricate coupling between hydrodynamic flows and particle surface properties.
By enabling dynamic control over both self-propulsion and assembly, our findings open up exciting possibilities for designing reconfigurable, high-density active systems with potential applications in smart materials, self-healing systems, and soft robotics. Additionally, our study lays the groundwork for further investigations into systems comprising mixtures of particles with varying self-propulsion speeds and inter-particle interactions. Finally, exploring the factors that govern the characteristic size of clusters at low frequencies will be a promising avenue for future research and the competition between the different components of electrohydrodynamic flows calls for further theoretical and numerical studies, as the low-frequency behavior of Janus active particles remains largely unexplored.
![]() | (1) |
| phase(ψ6) = arg(ψ6) | (2) |
) denotes the argument (or angle) of the complex number in the complex plane.
| B = A·J | (3) |
are the initial positions of the neighbors augmented with an additional column of ones to facilitate the inclusion of translational components. The matrix
contains the displacements after time step Δt, and
is the Jacobian matrix. To obtain the velocity gradients, eqn (3) was solved for J by calculating the dotproduct of B and the inverse of matrix A, A+. Finally, the vorticity ω was calculated as the difference between the partial derivatives of the velocity components:![]() | (4) |
Footnote |
| † Electronic supplementary information (ESI) available: Experimental videos and corresponding description. See DOI: https://doi.org/10.1039/d4sm01511h |
| This journal is © The Royal Society of Chemistry 2025 |