Masakazu
Kuze
ab,
Nozomi
Kawai
a,
Muneyuki
Matsuo
*ac,
Istvan
Lagzi
de,
Nobuhiko J.
Suematsu
bf and
Satoshi
Nakata
*a
aGraduate School of Integrated Sciences for Life, Hiroshima University, 1-3-1 Kagamiyama, Higashi-Hiroshima-shi, Hiroshima 739-8526, Japan. E-mail: muneyuki@hiroshima-u.ac.jp; nakatas@hiroshima-u.ac.jp
bMeiji Institute for Advanced Study of Mathematical Sciences (MIMS), Meiji University, 4-21-1 Nakano, Nakano-ku, Tokyo 164-8525, Japan
cGraduate School of Arts and Sciences, The University of Tokyo, 3-8-1 Komaba, Meguro-ku, Tokyo 153-8902, Japan
dDepartment of Physics, Institute of Physics, Budapest University of Technology and Economics, Muegyetem rkp. 3, Budapest H-1111, Hungary
eHUN-REN-BME Condensed Matter Physics Research Group, Budapest University of Technology and Economics, Muegyetem rkp. 3, Budapest H-1111, Hungary
fGraduate School of Advanced Mathematical Sciences, Meiji University, 4-21-1 Nakano, Nakano-ku, Tokyo 164-8525, Japan
First published on 12th March 2025
Oscillatory self-propulsion can be achieved under nonequilibrium conditions. In the case of a camphor boat, the periods of oscillatory motion were determined by the lateral (two-dimensional) transport length of camphor molecules at the solid plastic/water interface. However, the control of self-propulsion by different mass transport paths has not yet been explored. We observed new fluidic behaviors in the oscillatory motion of self-propelled objects. The period of oscillatory motion was determined by the mass transport path of the energy source molecules depending on the room temperature, Tr, and the temperature gradient, ΔT (= Tb − Tr, where Tb denotes the temperature at the bottom of the water chamber). We found that the oscillation period was determined by three types of mass transport paths for camphor molecules: lateral, downward, and complex. This study suggests that the three-dimensional transport path of energy source molecules can control the periods of oscillatory motion.
When a smaller camphor disk adhered to the basement and the center of a larger plastic disk floated on water as a self-propelled object named “self-propelled camphor object (SPC),” oscillatory motion between rest and motion was observed periodically.23–28 We previously reported that the period of oscillatory motion changes depending on the radius of the plastic disk, temperature, and viscosity of the water phase.25,28 In these studies, the periods of oscillatory motion were determined by the lateral (or two-dimensional) mass transport length of camphor molecules at the solid plastic/water interface.25,28 However, the control of self-propulsion by different mass transport paths, that is, the three-dimensional transport path, has not been explored.
In this study, we propose a simple self-propelled system using an SPC that is sensitive to the temperature conditions of not only the solid/water interface but also the water phase. Mass transport of camphor molecules in water was indirectly visualized using 7-hydroxycoumarin (7-HC) solid microparticles as a fluorescent indicator mixed in a solid camphor disk under UV light irradiation. We found three types of mass transport of camphor molecules; (1) lateral transport originated from the diffusion and the Marangoni flow by the difference in surface tension under a constant room temperature (Tr), (2) downward transport originated from the diffusion and the flow induced by the difference between densities of pure water and camphor solution under a constant Tr, and (3) complex transport originated from the diffusion and the thermal convection under the difference in the temperature, ΔT (= Tb − Tr, where Tb denotes the temperature at the bottom of the water chamber). The resting SPC accelerated when the camphor molecules reached the water surface from the water phase. In particular, we confirmed that the period of oscillatory motion is almost equal to the resting time. For types (1) and (2) under constant Tr, the period of oscillatory motion was determined by the ratio of types (1) and (2) depending on Tr. In type (3), for ΔT > 0, the oscillation period shortened with an increase in ΔT. We discuss the period of oscillatory motion in relation to the visualization of camphor molecules as a function of Tr and ΔT. These results suggest that the period of the oscillatory motion can be controlled not only by the two-dimensional mass transport of the energy source molecule around the solid/liquid interface but also the three-dimensional mass transport in the water phase, which was induced by ΔT.
The behaviors of the SPC under the absence and presence of temperature gradient in the water phase were monitored in experiments I and II, respectively. In experiment I, self-propulsion of the SPC and the camphor distribution at a constant temperature, Tr, were monitored from the top and side simultaneously. The SPC floated on water in the glass cell was examined in a fridge (Mitsubishi Electric Engineering Co., Ltd, SLC-25A, Tokyo, Japan, temperature range: 276–330 ± 1 K) to keep a constant value of Tr, as shown in Fig. 1b(i). To indirectly visualize the diffusion of camphor, UV light (wavelength: 365 nm, AS ONE Corporation, Handy UV Lamp UV-16, Tokyo, Japan) was irradiated, and the emitted light from 7-HC was monitored. In experiment II, the visualization of the camphor distribution and monitoring of the SPC were performed under the existence of a temperature gradient in the water phase, ΔT. Here, the glass cell was placed on the electronic thermostat (Matsuo Electronic Co. Ltd, METIII, Tokyo, Japan, the size of Peltier element: 50 mm × 50 mm) to control Tb, as shown in Fig. 1b(ii). Experiment II was performed in the cold room (Tr = 280 ± 1 K).
The motion of the SPC was monitored from the top and side views using digital video cameras (HDR-CX680, SONY, Tokyo, Japan; HC-W590MS-T, Panasonic, Tokyo, Japan; minimum time resolution, 1/30 s), and the images were analyzed using an image processing system (ImageJ, National Institute of Health, Bethesda, MD, USA). At least four examinations were performed under each experimental condition, and the SPC was replaced for each examination to confirm the reproducibility of the results.
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Fig. 2 Oscillatory motion of the SPC. (a) Time-variation on the speed of the SPC at Tr = (i) 280, (ii) 286, and (iii) 293 K in experiment I. The data obtained in (i), (ii), and (iii) are from the Movies S1, S2, and S3 in ESI,† respectively. (b) Time-variation on the speed of the SPC at Tb = (i) 286 K (ΔT = 6 K) and (ii) 293 K (ΔT = 13 K), respectively, in experiment II. Experiment II was performed in the cold room (Tr = 280 K). The data in (i) and (ii) were obtained from the Movies S4 and S5 in ESI,† respectively. |
Fig. 3a shows the period of oscillatory motion depending on Tr at ΔT = 0 K in experiment I. With an increase in Tr, the period of the oscillatory motion decreased in the range of 280–290 K; however, the period of oscillatory motion slightly decreased above 290 K. Fig. 3b shows the period of the oscillatory motion depending on ΔT at Tr = 280 K in experiment II. With an increase in ΔT, the period of oscillatory motion decreased in the range of 280–285 K; however, the period of oscillatory motion slightly decreased above 285 K. The period of oscillatory motion in experiment II was shorter than that in experiment I in the range of 283–288 K.
Next, the UV light was irradiated to the water phase to indirectly visualize the distribution of the camphor molecules dissolved from the camphor disk. Fig. 4 shows the time variation of the snapshots of the water phase during the resting state under different conditions of Tr and ΔT. At Tr = 280 and 286 K in experiment I, downward mass transport of camphor molecules from the disk to the base of the water chamber, in addition to lateral mass transport, was observed (Fig. 4a(i) and a(ii)). The amount of camphor that accumulated around the chamber base at Tr = 280 K (Fig. 4a(i)) was larger than that at Tr = 286 K (Fig. 4a(ii)). The downward mass transport was observed rather than the lateral transport at Tr ≤ 288 K. In contrast, lateral transport around the bottom of the plastic disk was mainly observed at Tr = 293 K in experiment I (Fig. 4a(iii)). When camphor molecules spilled from the edge of the plastic disk to the water surface, the resting object was accelerated.
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Fig. 4 Visualization of mass transport of camphor molecules around the SPC (side view). (a) Time-variation of snapshots at Tr = (i) 280, (ii) 286, and (iii) 293 K in experiment I. The corresponding snapshots in (i), (ii), and (iii) were obtained from the Movies S6, S7, and S8 (ESI†), respectively. (b) Time-variation of snapshots at ΔT = (i) 6 and (ii) 13 K in experiment II. The corresponding snapshots in (i) and (ii) were obtained from the Movies S9 and S10 (ESI†), respectively. The experimental conditions for (a) and (b) were the same as those for (a) and (b) in Fig. 1, respectively. The values beside the snapshots denote the elapsed time after the object was floated on the water surface (t = 0). A 1 wt% 7-hydroxycoumarin was mixed with camphor to visualize the distribution of camphor dissolved from the camphor disk under UV light irradiation. |
Fig. 4b shows the camphor distribution in the water phase at Tr = 280 K in experiment II. At ΔT = 6 K and 13 K, the downward transport of camphor molecules was mainly observed, and the direction of transport then changed upward. The resting object accelerates when the upward transport approaches the water surface.
Fig. 5 shows aqueous 7 mM camphor solution densities and those for water at different temperatures. At temperatures lower than 290 K, the density of the camphor solution tended to be higher than that of water. At temperatures higher than 290 K, the density of the camphor solution was similar to that of water.
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Fig. 5 Density of 7 mM camphor aqueous solution (empty circles) and water (filled circles) at different temperatures. Error bars represent the standard deviation obtained from the four examinations. |
We measured the light intensity at points A and B to evaluate the degree of the lateral and downward transport as a function of Tr. The light intensity at points A and B was measured just before the SPC accelerated from the resting state. Points A and B were 1 mm off from the edge of the camphor disk, as shown in Fig. 6a. Fig. 6b shows the light intensity ratio at point A (IA) to that at point B (IB), Ri (= IA/IB), as a function of Tr. Ri increased with an increase in Tr. The downward mass transport was clearly observed rather than the lateral transport in pure water at Tr ≤ 288 K. Here, we also investigated the light intensity in an aqueous NaCl solution to elucidate the effect of the density of the water phase on the nature of mass transport. When SPC was floated on 1.0 M aqueous NaCl solution, the lateral mass transport was mainly observed at Tr = 286 K and ΔT = 0 K (see filled circles in Fig. 6b). In this case, the period of the oscillatory motion of the SPC was 0.072 ± 0.017 h. This value was apparently lower than that on pure water (see Fig. 3a).
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Fig. 7 Schematic illustration of three types of the mass transport of camphor molecules depending on Tr and ΔT. |
First of all, three main mass-transport paths must be considered to understand the motion of the SPC (Fig. 4 and 7). First, the lateral mass transport of the camphor molecules originates from diffusion and the Marangoni flow, which is driven by the difference in surface tension due to the camphor concentration gradient around the SPC. Second, downward mass transport is generated by camphor diffusion and camphor sedimentation, originating from the density difference between the camphor aqueous solution and water. Third, convection is generated under a temperature gradient (ΔT > 0), contributing to the upward transport of camphor and helping the molecules reach the air/liquid interface faster. We note that this convection appears to be caused by the density instability driven by the vertical thermal gradient.
The period of the oscillatory motion at Tr ≥ 291 K and ΔT = 0 K was significantly shorter than that at Tr ≤ 288 K and ΔT = 0 K (refer to Fig. 3a). In previous studies, the period of oscillatory motion changed depending on the radius of the plastic disk and water temperature.23,25,27,28 The diffusion rate of camphor molecules in water depends on the temperature, and the period of oscillatory motion is determined by the time (ts) required to reach the threshold value of camphor molecules at the edge of the plastic disk to accelerate from the resting state.25 Therefore, ts at higher temperatures were shorter than those at lower temperatures. In addition, the density difference between the saturated camphor solution and water decreased with increasing temperature (Fig. 5). Fig. 5 and 6b suggest that the degree of the downward transport of camphor molecules generated by sedimentation at lower temperatures was greater than that at higher temperatures. Therefore, the ratio of the lateral transport of camphor molecules to the downward transport decreased with a decrease in Tr at ΔT = 0 (refer to Fig. 5). Consequently, the period of the oscillatory motion under ΔT = 0 at Tr ≤ 288 K is significantly longer than that at Tr ≥ 291 K. This is because it takes a long time to reach the threshold value to obtain the acceleration owing to downward diffusion. Consequently, oscillatory motion with an extended period (∼1.8 h) was observed at Tr = 280 K and ΔT = 0 K.
Next, we discuss the mass transport paths of the camphor molecules at ΔT > 0. The convective flow around the SPC at Tr = 280 K and 0 < ΔT ≤ 13 K is generated by the Marangoni flow due to the existence of ΔT.29 The period of oscillatory motion depending on Tb at Tr = 280 K is shorter than that depending on Tr at ΔT = 0 in the range of 282–288 K (refer to Fig. 7). This result suggests that the time for camphor molecules to reach the water surface owing to convective flow is shorter than that required to reach the edge of the plastic plate owing to lateral transport. Large values of ΔT may induce shorter periods of oscillatory motion owing to rapid convective flow. However, the period of oscillatory motion at Tb ≥ 291 K and ΔT ≥ 11 K was similar to that at Tr ≥ 291 K and ΔT = 0 K (refer to Fig. 7). This is because the downward flow was weakened by the low-density difference (Fig. 5), and the period of the oscillatory motion was determined by lateral transport at temperatures higher than 291 K. Fig. 6 suggests that behaviors of the SPC and mass transport of camphor molecules were strongly affected by the density difference between the water phase and dissolved camphor solution.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4cp04832f |
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