Amir
Kashani
and
H. Jeremy
Cho
*
Department of Mechanical Engineering, University of Nevada, Las Vegas, Las Vegas, NV 89154, USA. E-mail: jeremy.cho@unlv.edu
First published on 1st December 2023
Wetting and water absorption of hydrogels is often encountered in many applications. We seek to understand how wetting behavior can be affected by the time-dependent swelling of hydrogels. We measured the advancing contact angles of water droplets on hydrogels of varying thicknesses where thicker gels absorbed water more slowly. We also observed that, above a threshold advancing speed, water droplets would collapse into a lower contact angle state on the surface. We hypothesized that this collapse threshold speed is a result of competition between the poroelastic diffusion of water into the gel and the advance of the spreading droplet, the thickness of the surface, and the diffusion of water into the gel. Taking the ratio of the diffusion and advancing timescales results in a Peclet number with gel thickness as a characteristic length scale. Our results show that above a Peclet number of around 40, droplets will collapse on the surface across all gel thicknesses, confirming our hypothesis. This work provides simple insight to understand a complex time-dependent wetting phenomenon for a widely used hydrogel.
Based on numerous studies, the wettability of hydrogels depends on its swelling state17 where more de-swollen gels tend to be more hydrophobic compared to swollen gels.18 However, there are limited tools to predict, quantify, or model these dependencies. One way to quantify wettability is through the contact angle, which is the angle a droplet makes with the surface at the contact line. The contact angle has a maximum when the droplet is advancing, θadv, and a minimum when the droplet is receding, θrec.19 Typically, wetting behavior is not time-dependent in that advancing and receding contact angles do not change over time. However, in the case of hydrogels that swell with water, during the course of a water droplet being in contact with the surface, water will diffuse into the gel, causing contact angles to decrease over time.20
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Here, the prefactor κK/μ is the poroelastic diffusion coefficient,
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Measuring Dpe requires obtaining the values of permeability, κ, and stiffness, K, independently. To measure permeability, we previously developed a flow-cell technique to drive water through thin gel samples.22 Using Darcy's law, we are able to calculate the permeability from the measured flow rate and applied hydraulic pressure. We used polyacrylamide (PAAm) hydrogels with methylenebisacrylamide (MBA) as a crosslinker (further details in ESI†). For 1-%-crosslinking (mol crosslinker/mol monomer) used in this study, we measured a permeability (5.2 ± 0.5) × 10−18 m2. Polyacrylamide gels were chosen as they are easily made and are extremely ubiquitous from contact lenses23 to enhanced oil recovery.24 To measure stiffness (bulk modulus), we performed compression testing of hydrogel samples using a spherical indentation tester.25 Using Hertzian theory, we can determine Young's modulus from applied displacement and measured compressile load. Assuming that Poisson's ratio is 1/3 as is typical for hydrogels,25–28 the bulk modulus is equal to the Young's modulus, K = E. For 1-%-crosslinking (mol crosslinker/mol monomer), we measured a bulk modulus of (15.1 ± 1.6) kPa. Since the viscosity of water is known, we can calculate the poroelastic diffusion coefficient to be (8.4 ± 1.2) × 10−11 m2s−1. Previously, we investigated the changes in permeability and stiffness with crosslinking and found that any changes in permeability are nearly inverse with any changes in stiffness.22 Thus, across different crossslinker ratios, the poroelastic diffusion coefficient remains relatively constant, as shown in Fig. S1 (ESI†).
As mentioned earlier, water can diffuse into a gel and affect its wetting properties over time.20 Since we can quantify the poroelastic diffusion coefficient, we can also quantify the characteristic diffusion time, tdiff of water diffusing into the gel as
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Fig. 1 As a droplet advances with a speed of V, water diffuses into the permeable gel substrate with a thickness L. |
To verify this time scale, we conducted a simple experiment where we placed a water droplet on a ∼80 μm-thick sample and observed swelling of the gel. For this thickness, the characteristic diffusion time scale is approximately 90 s. As shown in Fig. 2, the diffused water swells the gel underneath the droplet and forms a “foot” in a time scale that is within the same order of magnitude of the tdiff. We further verified this time scale through a series of finite-element-method (FEM) simulations. We applied Fick's second law and linear elastic theory (using our previous methodology29) where the diffusion coefficient is Dpe. We simulated gels of various thicknesses and performed transient simulation of swelling in response to a wet boundary condition on the top of the gel. Remarkably, the time to 90% swelling at the bottom of the gel after exposure at the top coincided with the diffusion time scale, L2/Dpe, to within 6% (Fig. S2, ESI†).
To probe the wetting behavior, we sought to measure the advancing contact angle of the gel surface. This involves growing a droplet of DI water on the gel using a dispensing needle where the pressure of the liquid was controlled by a microfluidic pressure regulator (Elveflow OB-1). However, due to the simultaneous diffusion occurring, we would expect different values of contact angle depending on advancing speed. Indeed, when very high advancing speeds were applied, we observed that a droplet would collapse, as shown in Fig. 3. This collapse event is a sudden change in the shape of the droplet with a jump in droplet base radius and an immediate lowering of the apparent contact angle. We only observed this collapse when fast advancing speeds were applied.
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Fig. 3 (a) Advancing of a droplet on top of a 0.5 mm-thick (Lwet) gel substrate before the collapse. (b) At some point, due to the high advancing speed, a sudden decrease in the contact angle occurs, which is referred to as the collapse of the droplet (Video S1, ESI†). |
To understand the reason for this collapse, we calculated a range of possible spherical droplet geometries on top of a foot-shaped surface modeled using a sinusoidal S-curve where the droplet conserves a fixed advancing contact angle over the surface (Fig. 4). As the droplet contact line advances over the lip of the periphery edge of the foot, the apparent contact angle increases as a result of the surface sloping downward. We noticed that there is a local maximum in droplet volume at this foot periphery edge. At this critical point, there would be no way to add an infinitesimal amount of volume and expect an infinitesimal increase in droplet base radius since the volume decreases since the slope of volume versus base radius is negative immediately after the maximum point. Thus, the only possible way to continue to add volume is for the base radius to jump to a much higher value (arrow in Fig. 4), hence the collapse phenomenon. In agreement with our experiments, the apparent contact angle decreases immediately after collapse as there is no downward-sloping foot periphery edge to increase it over the intrinsic advancing contact angle. We have performed this analysis for several contact angles and found similar results (Fig. S3, ESI†). In addition, we have included an animation sequence of the simulated collapse phenomenon (Video S2, ESI†). We also confirmed that this collapse behavior is unique to swelling gel substrates as we did not observe any collapse on an impermeable surface using our experimental setup (Fig. S4, ESI†). In addition, no evidence of any liquid film formation either at the top or bottom was observed.
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Fig. 4 Simulated droplet geometry over a modeled foot shows that collapse over the periphery edge of the foot must occur in order to preserve the volume. An animation of this simulated collapse event is presented in Video S2 (ESI†). Arbitrary units are used for length. |
Thus, in order to prevent collapse, the foot should grow radially outward with the advancing droplet. For foot growth to happen, diffusion into the gel must be sufficiently fast to keep pace with the speed of advance. We suspected that the collapse occurs when the time scale of droplet advance becomes shorter than the time scale of diffusion, tadv < tdiff. From simple dimensional analysis, we can define an advancing time scale as
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When Pe is high, the rate of advance is faster than the rate of diffusion and we would expect droplet collapse to occur. Thus, we hypothesized that above a critical Peclet number, droplet collapse occurs whereas below the critical value, droplets advance stably. We illustrate the hypothesized behavior in Fig. 5 where from a droplet over a formed foot (panels a–c), either the droplet collapses if the advancing speed is too high (d) or the foot grows with the advance, preventing collapse.
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Fig. 7 An example of the measured base diameter and contact angle over time for the droplet where collapse occurred (Video S1, ESI†). The thickness was 0.5 mm and the advancing speed was 0.35 mm min−1. |
Once a foot was developed (Fig. 5a and b), we proceeded to advance the droplet contact line at prescribed speeds to double the droplet base diameter. In all trials, either one of two events occurred: (1) the droplet advanced to twice the initial base diameter with no collapse and a stable advancing contact angle (Fig. 6) or (2) the droplet collapsed at some point in time during the advance (Fig. 7). In the cases where droplets advanced stably, apparent advancing contact angles were measured as functions of thickness and speed as shown in Fig. S5 (ESI†) with full data in Table S1 (ESI†). The thinnest samples had slightly lower contact angles, which may be due to faster swelling causing the droplet to appear more hydrophilic. There was also a trend of contact angle slightly decreasing at higher advancing speeds, which may signify proximity to a collapsed state; however, this trend is not very significant given the uncertainty in measurements. In the cases where droplets collapsed, we observed a sharp decrease in contact angle and the trial was terminated (Fig. 7).
To obtain useful statistics to determine the threshold advancing speed for collapse, we repeated trials at each combination of thickness and speed at least three times. The outcomes, expressed as a ratio of collapse events over number of trials, are shown in Fig. 8. This ratio represents a probability of collapse. From these probabilities we created a heat map to visualize the distribution of probabilities as a function of thickness and speed. We noticed that there is a boundary between the no-collapse region in the bottom-left and the collapse region in the top-right. This boundary resembles an inverse relationship between advancing speed and thickness. This inverse relationship can be derived from the Peclet number, Pe = LV/Dpe. If we set Peclet number to a fixed threshold value as we hypothesized and solve for V, we obtain V = PeDpe/L, which is an inverse function with L. For experimental convenience, we use the wet-state thickness L = Lwet since these thicknesses are more easily measured at the reference wet state. Since Dpe is known for our samples, we fit a value of Pe such that the function V = PeDpe/Lwet overlapped with the boundary between collapse and no-collapse regions. We found this threshold value of Peclet number to be around 40. Thus, we confirm that above a certain Peclet number, collapse of the droplet occurs.
To gain a more physical understanding of why the competition of diffusion versus advection, as quantified by the Peclet number, dictates collapse versus stable-advance behavior, we performed FEM simulations that resemble our experiments. Here, a dry gel of thickness Ldry = 80 μm was the simulation domain with a wet boundary condition, resembling a droplet, being applied. The droplet base radius was initially set to 0.5 mm for a period of tdiff = Ldry2/Dpe = 79 s to form the foot in accordance with experimental procedures (Fig. 5a and b). A foot does indeed form as shown in Fig. 9a. Interestingly, the foot periphery edge extends outward beyond the contact line due to the fact that diffusion is occurring simultaneously in the downward (negative y) and outward, radial (positive x) directions as indicated by the water flux arrows. After initial foot formation, the boundary condition was expanded at either a rate of 2 mm min−1, 0.2 mm min−1, or 0 mm min−1, corresponding to Peclet numbers of 63, 6, and 0. At a high Peclet number of 63, the rate of advance is high such that diffusion toward the bottom of the gel does not complete, leading to a thin section of swelling (Fig. 9b, blue region) over a large, dry region (red region). Since much of the region underneath the newly wetted top surface remains dry, only a small change in foot geometry results. As our simulations of droplet geometry over a foot show (Fig. 4), collapse would occur over a foot that does not expand with the advance. Thus, the high-Peclet situation in Fig. 9b would likely result in collapse, as our experimental results would suggest. Conversely, in the low Peclet number of 6 case, diffusion is able to keep pace with advance, leading to a more uniform concentration distribution as shown in Fig. 9c. As a result, the gel is much more swollen under the newly wetted region and the foot periphery edge remains ahead of the contact line, leading to a likely stable advance of the droplet, in agreement with our experiments. Finally, as a control where Pe = 0, we observe that diffusion is very slow as the concentration distribution in Fig. 9d is nearly identical to Fig. 9a—though given infinite time, the gel would fully swell with water everywhere assuming evaporation is minimized. This means that the radial spread of water is driven by the moving wetted boundary condition (advancing droplet) and its corresponding diffusion at the downward and outward directions over a length scale of the gel thickness. In the simulation, we did not consider effects of capillary pressure from droplet curvature and gravity affecting transport because these can be shown to be three to five orders of magnitude smaller than the osmotic driving forces that cause water to diffuse into the gel (see ESI,† Section 3). Thus, the rich physical picture that the FEM simulations provide is completely consistent with what we observed in our experiments regarding collapse versus stable advance.
• Acrylamide (AAm)
• N,N′-Methylenebis(acrylamide) (MBA)
• Ammonium persulfate (APS)
• N,N,N′,N′-Teramethylethane-1,2-diamine (TEMED)
All chemicals used in this paper were purchased from Sigma-Aldrich Co.
All hydrogels were prepared in a similar fashion to our previous work.22,25 We start from aqueous stock solutions of the following chemicals: N,N′-methylene(bis)acrylamide (MBA), ammonium persulfate (APS), and tetramethylethylenediamine (TEMED) at concentrations of 0.1084 g/10.0 mL, 0.0800 g/10.0 mL and 0.250 mL/10.0 mL, respectively. The base acrylamide (AAm) monomer was used in its pure powder form. By mixing specific amounts of these chemicals and DI water, polymers were spontaneously synthesized. During this process, APS served as an initiator, TEMED as an accelerator, and MBA as a crosslinker. Hydrogel stiffness could be varied from 7 to 31 kPa using different crosslinking amounts ranging from 0.5% to 5% (mol MBA per mol AAm). However, according to our previous study,22 we found that the resulting poroelastic diffusion coefficient is largely invariant with crosslinking. Hence, we chose a “middle-of-the-road” crosslinker amount of 2% since it is the center of the previous testing range and would represent where we understand the hydrogel behavior best.
In all hydrogel samples, we started with 0.500 g of AAm monomer, 0.025 mL of TEMED solution, 1.00 mL of APS solution, and 1.00 mL of MBA solution to achieve the target crosslinker ratio (mol crosslinker/mol monomer) of 1.00%. The mixed solutions were poured into molds with 0.79 mm, 0.50 mm, and 0.25 mm thicknesses by using smooth slide glass for the top and bottom surfaces of the mold and subsequently polymerized for 24 hours. Then, the samples were immersed in DI water for one week to remove unreacted chemicals and equilibrate them to the wet state. Finally, samples were kept in the lab ambient air for 24 hours to dry completely. The lab ambient air was at a relative humidity of around 15% to 30% and a temperature of 23 °C. Mirror-like specular reflections were visible on the surface as shown in Fig. S6 (ESI†), indicating that roughness effects were minimal.
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Footnote |
† Electronic supplementary information (ESI) available: Supplementary information, table, and video. See DOI: https://doi.org/10.1039/d3sm01472j |
This journal is © The Royal Society of Chemistry 2024 |