Dimitri Radajewski,
Pierre Roblin,
Patrice Bacchin
,
Martine Meireles
and
Yannick Hallez
*
Laboratoire de Génie Chimique, Université de Toulouse, CNRS, INPT, UPS, Toulouse, France. E-mail: yannick.hallez@univ-tlse3.fr
First published on 10th April 2025
We have developed a microfluidic chip for the osmotic compression of samples at the nanoliter scale, enabling the in situ and operando acquisition of structural features through small-angle X-ray scattering throughout the compression process. The design builds upon a previous setup allowing high-throughput measurements with minimal sample quantities. The updated design is specifically tailored for compatibility with a laboratory beamline, taking into account factors such as reduced photon flux and increased beam size compared to synchrotron beamlines. As a proof of concept, we performed on-chip compression of well-documented silica colloidal particles (Ludox TM-50). We demonstrated that the volume fraction could be tracked over time during compression, either by monitoring X-ray absorbance or by modeling the scattered signal. With precise control of the osmotic pressure and salt chemical potential, equations of state can be determined unambiguously from the volume fraction measurements and be interpreted with the help of the scattered intensity. These microfluidic chips will be valuable for understanding the behavior of colloidal suspensions, with applications in areas such as crystallization, nucleation, soil mechanics, control of living matter growth and interaction conditions, as well as the measurement of coarse-grained colloidal interaction potentials.
Osmotic compression has been widely used to characterize colloidal dispersions. The osmotic stress technique is a well-established method in which a dilute dispersion is placed in a dialysis bag, which is then immersed in a bath containing salt and polymers imposing the chemical potential of water. The bag is impermeable to polymers and colloids, but allows solvent and ion exchange.7–11 Over time, solvent and ions gradually transfer through the membrane, leading to the concentration of colloids until thermodynamic equilibrium is reached. Key advantages of the osmotic stress technique include its ability to produce concentrated and homogeneous states without requiring a possibly complicated mixing step, as well as its precise control over both the chemical potential of water in the dispersion (or equivalently, the osmotic pressure of the dispersion Π) and the chemical potential of ions, which dictates the electrostatic interactions between colloids. Other methods allowing the observation of colloidal dispersions at different volume fractions and the measurement of osmotic pressure include in particular the exploitation of sedimentation profiles with or without centrifugation.12
The evolution of the osmotic pressure as a function of the colloid volume fraction ϕ at equilibrium, for fixed temperature and ion chemical potential, is the equation of state (EOS) of the dispersion. The EOS serves as an indirect signature of colloidal interactions, and comparing it with existing thermodynamic models allows, to some extent, to determine effective inter-particle potentials.13,14 These potentials are critical for further calculations, such as predicting mass transport in drying processes15,16 or modeling flows in dense suspensions.17,18 Another key application of the osmotic stress technique is the ability to provide access to the phase diagram of colloidal dispersions: for samples prepared in different physico-chemical conditions, fluid, glassy, or crystal microstructures can be identified with high resolution scattering methods, such as small angle X-ray scattering (SAXS), often performed on synchrotron beamlines.15,19 The phase diagrams are then built in a parameter space where independent axes can be the volume fraction, the salt concentration in the bath cres, and the dimensionless charge or reduced temperature.8,20–23 In charge regulating systems such as metal oxides or proteins, this last parameter can be replaced by the pH.
While the osmotic compression technique offers significant advantages, it also has several limitations. First, for nanometric-sized colloidal dispersions, reaching equilibrium in a centimeter-wide dialysis bag can require an extended duration, typically several weeks.24 During this time, the bath must be regularly replaced to maintain constant pH and salt/polymer concentrations, which can be labor-intensive. Second, the final volume of the dialysis bags must be sufficiently large, typically several milliliters, to allow for sample extraction, weighing, and transfer to X-ray cells. This can be problematic for costly or dilute samples, such as some RNA or quantum dot dispersions. Third, transferring samples from dialysis bags to capillaries or other X-ray cells for SAXS experiments often introduces uncertainty due to the significant shear forces experienced during pipetting and injection.23,25 These forces can alter the microstructure of the colloidal dispersions, potentially preventing the samples from relaxing to their original state before the X-ray measurements are taken.
Microfluidics offers a promising solution to address some of the challenges associated with the well-established osmotic compression technique. It provides advantages such as minimal sample volume requirements, high-throughput measurements, and reliable in situ structural analysis over a broad range of pH, salt concentrations, and colloid volume fractions. Recently, a significant advancement in this field has been introduced. A microfluidic chip replicating the osmotic stress technique has been developed to measure the equation of state of charged dispersions.24 This setup reduces the sample volume to the nanoliter scale, drastically shortening equilibration times to just a few minutes. EOS measurements were conducted on charged polystyrene particles at volume fractions up to 0.4 and under varying salt concentrations, demonstrating good agreement with liquid-state theory. In this study, fluorescence was used to determine the colloidal volume fraction as a function of the imposed osmotic pressure. However, the suspension microstructure could not be analyzed as the chip was not compatible with X-ray scattering techniques. In the last few years, microfluidic devices designed for in situ SAXS measurements of colloidal dispersion microstructure using a laboratory beamline have been introduced.26,27 We measured structural properties of different colloidal dispersions with varying electron densities to assess the capabilities of such setups.27 However, unlike the microfluidic chip in ref. 24, this device did not allow in situ compression.
Building on these recent advancements, we have developed a new microfluidic chip implementing osmotic compression as demonstrated in ref. 24, but also allowing in situ and operando SAXS measurements. In doing so, the chip design has been specifically tailored to ensure compatibility with laboratory beamlines, accounting for factors such as a moderate photon flux and a larger beam size compared to synchrotron sources, following ref. 27. We illustrate this approach with the microfluidic compression of well-documented silica colloidal particles (Ludox TM-50)15,19 which are widely used as model systems for advancing the fundamental understanding of drying processes in coated films. In the following sections, we provide a detailed description of the microfluidic chip, the process for synthesizing a membrane inside it, and the SAXS laboratory beamline. We then illustrate how structural analysis of the dispersion can be performed to identify different phases and demonstrate how the volume fraction can be reliably monitored in time to study compression kinetics and derive equations of state.
![]() | ||
Fig. 1 Central part of the microfluidic setup with a drop of colloidal suspension trapped on the membrane. The size of the X-ray beam (250 μm) is represented approximately. The hatched portion of the Kapton film was present in the main experiment reported here, but could be removed in the preliminary experiment reported as ESI.† |
Fluids and suspensions could flow in and out of the device using PEEK capillaries (360 μm OD, 150 μm ID, Trajan Scientific, United Kingdom) used as connectors and glued to the inlet and outlets of the chip with epoxy. These capillaries were then connected to Flow EZ pressure controllers (Fluigent, France) with 1/16′′ OD PTFE tubing with specific adapters.
To synthesize the nanoporous membrane, an aqueous formulation containing PEGDA700, 2-hydroxy-2-methylpropiophenone as photo-initiator, and PEG1000 as a pore-forming component was first injected everywhere in the microfluidic device. Spatially resolved photo-polymerization was then employed to cross-link a hydrogel slab at the end of the transverse channel (see Fig. 2).24,31 UV exposure was carried out with the HXP 120 C lighting unit of an AXIO ObserverZ1 inverted microscope. The shape and the size of the area exposed was controlled with a variable rectangular diaphragm (1140-737, ZEISS, Germany) positioned on the optical path of the lamp and reproduced on the focal plane of the microscope through a 20× objective. The microfluidic chip was positioned such that the slit illuminated only a small rectangular area at the end of the transverse channel, precisely forming the membrane after a few seconds of exposure. The chip was then cleaned by flushing it with pure water for a few hours to remove the non-polymerized solution completely.
The membrane demonstrated strong anchoring to the OSTEMER walls, withstanding trans-membrane pressures up to 6 bars during cleaning. An overview of the membrane formation process is presented in a video in ESI.† Note that attempts to synthesize membranes directly in 300 μm high channels proved unreliable. While cross-linked regions were formed, the colloidal suspension often leaked through them due to poor homogeneity and incomplete attachment to the walls. It may be because the channel thickness was much larger than the thickness of the focal plane, so UV illumination was uneven vertically, and therefore insufficient in certain regions. Introducing a 250 μm-high step in the channel and synthesizing a 50 μm-high membrane on top of it resolved this issue. One drawback of this approach is the reduced membrane surface area for water transfer, leading to slower compression kinetics.
The colloidal suspension was injected at inlet A until it invaded the AB channel and the transverse channel. A 500 mbar pressure was applied, allowing the suspension to displace the water in the transverse channel through the membrane. During this step, several SAXS images were taken at different positions along the transverse channel and into the AB channel to confirm the colloid concentration was uniform. An immiscible oil (AR20, Sigma-Aldrich) was then injected at inlet A to flush the colloidal suspension from the AB channel, leaving a drop of the suspension confined in the transverse channel, as illustrated in Fig. 1.
Compression experiments started at this stage. The flow of salt solution was maintained in channel CD to ensure a constant salt concentration and pH on the opposite side of the membrane. Two pressure controllers then imposed identical pressures to the oil at inlets A and B, with values ranging from 100 mbar to 2 bar. In response, solvent from the colloidal droplet was pushed through the membrane and the colloids were concentrated until mechanical and chemical equilibrium was achieved. The imposed pressures were sufficiently high to disregard the capillary pressure of the droplet meniscus (<10 mbar) and the pressure driving the flow of the salt solution in the CD channel (<10 mbar). A preliminary experiment, reported in ESI,† was performed with a low salt concentration to validate the geometry of the microfluidic chip and to evaluate the time scale for equilibration at different set pressures. The experiment described in this article was performed with a different salt and ionic strength, allowing comparison with extensive data obtained by Goehring and coworkers using classical osmotic compression.15,32
This process yielded the intensity profiles Is(q). The background scattering profile, Ib(q), was determined from SAXS images of the transverse channel filled initially with the buffer solution, following the same standardized scaling procedure. The final intensity profiles reported hereafter are defined as I(q) = Is(q) − Ib(q). Under the assumption of single scattering, they can be expressed as
I(q) = AϕP(q)Sm(q) | (1) |
![]() | ||
Fig. 3 SAXS patterns obtained during experiment 2. From left to right: (a) initial dispersion before compression, ϕ = 0.085; (b) after 60 minutes in the course of the first compression step, ϕ = 0.125; (c) after 300 minutes in the course of the first compression step, ϕ = 0.246 ± 0.006; (d) equilibrated state after 15 hours at the end of the first compression step at a pressure equal to 0.1 bar, ϕ = 0.242 ± 0.004; (e) equilibrated state at the end of the second compression step at set pressure equal to 0.15 bar, ϕ = 0.288 ± 0.005; (f) equilibrated state at the end of the third compression step at a pressure equal to 0.2 bar, ϕ = 0.335. (a) and (b) are liquid phases, (c)–(e) are a mix of BCC crystallites and an amorphous background, and (f) is essentially a glass with traces of BCC crystallites. The long equilibration times compared to those reported in ref. 24 are discussed in section Compression kinetics. |
Azimuthal averaging of the 2D pattern measured before compression (Fig. 3(a)) yields the 1D spectrum reported in Fig. 4. The main features of this spectrum are classical ingredients for repulsive, charge-stabilized colloidal dispersions: the intensity drops at low q due to the weak compressibility, the principal peak at q ⋍ 0.015 is a structure peak reminiscent of inter-cage distances, and the oscillations for q > 0.03 stem essentially from the form factor of spherical and slightly polydisperse colloids.
This spectrum has been fitted using eqn (1) with the following models for P(q) and Sm(q). Polydispersity has been accounted for using a Gaussian distribution for the radii in the form factor, which involves an average radius a and a polydispersity index. Computing a measurable structure factor is more involved. First, an effective interaction potential needs to be determined. Here we use a hard-sphere-Yukawa model ueff depending on an effective colloidal charge Zeff and on an effective screening length κeff−1. These quantities were determined using a Poisson–Boltzmann (PB) cell model33,34 for a monodisperse suspension of colloids with a radius equal to the average radius a. A simple one pK Stern model of colloidal surface chemistry was implemented in this cell model, so the bare surface charge density and the electrostatic potential around a colloid were computed self-consistently as a function of salt chemical potential and pH considering the surface reaction
Si–OH ⇌ Si–O− + H+, |
The measurable structure factor Sm(q) was then estimated as the structure factor S(q) of a monodisperse suspension of colloids with a radius equal to the average radius a at the same volume fraction. This function was obtained by solving the Ornstein–Zernike equation with the effective potential ueff and the hypernetted-chain (HNC) closure. Identical results are obtained using the rescaled mean-spherical approximation (RMSA). We also tested a decoupling approximation37,38 to include polydispersity effects in the structure factor calculation but it did not improve the results significantly. The monodisperse model S(q) was therefore used throughout this work for simplicity (see the ESI of ref. 27 more details concerning this approach).
Optimization of the free parameters of this model with respect to the SAXS data obtained before compression allowed to determine the average particle radius a = 14.2 nm, the size polydispersity 1.46 nm, the initial volume fraction of the suspension ϕ = 0.0822, and a pH of 9.02, which matches well the pH at which the suspension was prepared (pH = 9). These parameters yield an initial surface charge density of σ = 0.421 e nm−2. The result of the fitting procedure matches the experimental data very closely (see Fig. 4). For comparison, Goehring and coworkers reported an average radius between 13.3 and 14.1 nm using different techniques and an identical polydispersity of 10%.15,39
With the form factor measured in the “dilute” initial state, the structure factors of the suspension at higher volume fractions, after equilibration at 100, 150, and 200 mbar, could be extracted from the scattered intensities. They are reported in Fig. 5, together with one measurement by Chang and coworkers23 which was conducted in conditions very close to those of our experiment at 100 mbar. Note that the experiment of Chang et al. was conducted on a synchrotron beamline, after weeks of classical osmotic compression. In both the present experiment at 100 mbar and Chang and coworker's experiment, we observe an essentially liquid-like structure with additional bumps located at the positions of the peaks of a body centered cubic (BCC) crystal. Such a structure has also been discussed by Bareigts and coworkers32 on the TM50 colloids used here. A notable difference between the structure factors reported by previous authors23,32 and the one measured in the present microfluidic chip is the width of these additional BCC peaks. The peaks in the preliminary experiment at cres = 1 mM reported in ESI† were thinner than those from the experiment reported here although the same X-ray beam and the same colloids were used. This rules out the influences of beam collimation and of polydispersity. The width of secondary peaks may also be influenced by the size of the crystallites. Here the half-width-half-maxima value δ ≃ 1 × 10−3 would suggest a crystallite size about π/δ ≃ 300 nm, which is outside the q range accessible by SAXS. The thinner peaks visible on Chang's curve would correspond to crystallites in the micrometer range. It could be possible that the time scale of our experiment did not allow to reach the same crystallite size as the one reported in ref. 23.
![]() | ||
Fig. 5 Structure factors measured (crosses) and computed with liquid theory modeling (lines) ignoring the eventual existence of crystallites. The black dotted lines indicate the first theoretical BCC peak positions. The reservoir salt concentration was cres = 5 mM, so κresa = 3.34. The dashed blue curve was taken from Fig. 10 in Chang et al.23 for comparison, where ϕ = 0.23 and κresa = 3.33 (a = 10 nm, polydispersity 1.3 nm, cres = 10 mM). |
At a higher osmotic pressure of 150 mbar (and ϕ = 0.288), these peaks are barely discernible, and at 200 mbar (ϕ = 0.336) they seem to have completely disappeared. This crystal-to-glass transition upon concentration increase is consistent with previous results obtained on out-of-chip synchrotron runs and simulations, where the transition was found around ϕ = 0.25 at cres = 5 mM.32 Predictions from the liquid theory are also reported in Fig. 5. They were obtained by fitting the volume fraction so the main peak position qmax is located at the correct q value, and by fitting the pH so the osmotic pressure in the model corresponds to the one imposed in the chip. The liquid theory model overestimates the main and secondary peak amplitudes because it cannot account for the presence of slightly denser and more ordered crystallites but it is consistent with the peak positions of the amorphous matrix.
The volume fractions reported above were determined by fitting the liquid theory model on the measured scattered intensities. Using this approach systematically on the different SAXS spectra obtained as a function of time yields the volume fraction evolution reported as a black curve in Fig. 6. The sometimes rough nature of this curve comes from the automatic fitting algorithm used on the ∼200 structure factors analyzed. As the present suspension sometimes contains BCC crystallites, we also used the relation
![]() | ||
Fig. 6 Volume fraction ϕ as a function of time during compression in the microfluidic chip. The different line colors correspond to different approaches to estimate the volume fraction, as described in the text. The black circles correspond to the 2D SAXS patterns reported in Fig. 3. Their ϕ value is the average of the “liquid” and “BCC” values. |
Note that measuring ϕ by fitting the liquid theory to the SAXS spectra was achievable, though time consuming, because we utilized a well-known system of spherical, nearly monodisperse colloids for this proof of concept. However, the true value of exploring phase diagrams of colloidal suspensions using a microfluidic chip lies in studying systems that are not well understood, where a theoretical model is likely unavailable. Therefore, we will now discuss another approach to measure the colloid volume fraction.
A simple method to determine the volume fraction with the X-ray data is to compute the X-ray absorption based on the measured incident intensity I0 and the transmitted intensity I(t) for each image. The absorbance follows Beer–Lambert's law
A(t) = ln(I0/I(t)) = c + μwh(1 − ϕ(t)) + μshϕ(t), | (2) |
![]() | (3) |
Except when the volume fraction estimation based on absorbance fluctuates strongly for times larger than 50 hours, the difference between the three volume fraction estimations obtained with the different models was generally less than ±0.02 so the measurements were quite robust and consistent here.
Note that this time scale to reach equilibrium is much larger than the 5 to 30 minutes achieved in our previous work using microfluidic osmotic compression without the constraints of in situ SAXS analysis.24 Indeed, changes in the chip geometry were required to perform the SAXS experiments on a laboratory beamline: the initial colloidal drop length has been increased from 0.6 mm to 3.6 mm to allow the 0.25 mm beam size to fit into the drop even after a ten-fold compression, and the channel depth has been increased from 50 to 300 microns to increase the scattered to background intensity ratio. Therefore the volume of fluid to be exchanged through the membrane during a compression in the present chip was about 36 times larger than what could be realized without these constraints, while the membrane surface area involved in the exchange remained the same. Since at these small scales the water transfer kinetics are limited by the membrane permeability,24 a 36-fold water volume increase induces a 36-fold transfer time increase, which is consistent with what was observed. Note that the present increase in drop size and channel depth were necessary to use a laboratory beamline, but a synchrotron X-ray source is much brighter and with a more focused beam so the present chip modifications would not be necessary in this context, and compression could be achieved in a few minutes with in situ micro-structure measurements. Finally, note that even if a compression step requires about 20 hours here, the device still allows for a continuous acquisition for different compression steps with a unique sample, without pipetting events that might disturb the micro-structure of the dispersion. It is therefore still a very valuable tool for the high-throughput screening of new colloidal formulations.
To compute the osmotic pressure, we first compute the suspension meso-structure (in the form of S(q) or g(r)) by solving the OZ equation with an effective potential determined as introduced above. The osmotic pressure is then36
![]() | (4) |
The Π(ϕ) data sets measured at equilibrium in microfluidic chips are reported in Fig. 7 for two different salt reservoir concentrations, together with theoretical results. The initial states (volume fractions) of the dispersion drops at cres = 1 and 5 mM introduced inside the microfluidic chips are indicated with blue and red crosses, respectively. They were purposely set quite far from the equilibrium values, and arrows show the path followed by the dispersion during compression inside the microfluidic chip. Open circles are the stationary states obtained for each pressure step. For the experiment reported in red, the salt solution in the reservoir was prepared at pH = 10 and cres = 5 mM. Agreement is very good with theory at pH = 10 for the first pressure step at 100 mbar reached after 17 hours, as expected. The volume fractions reached during the next two pressure steps at 150 and 200 mbar and obtained after 40 and 60 hours of compression appear to lie on equations of state corresponding to pH = 8.5 and 7.75, respectively. These results suggest a slow acidification of the salt reservoir with time. This is confirmed in the experiment at cres = 1 mM reported in blue, where the first two data points are in good agreement with the theoretical values taken at pH = 10. The first data point was obtained after 27 hours of operation, and the second point was obtained after approximately 10 hours of aging the salt solution, following a refill of the salt reservoir in between. The final data point in this experiment appears to align with the equation of state for pH = 8.3, after 80 hours of aging the salt solution.
Water acidification due to CO2 absorption is well known when it is left exposed to the atmosphere but we did not expect this to occur in the closed Fluigent pressurization cells. The pH was therefore not monitored during the compression experiments, but pH measurements have been conducted a posteriori in pressurized and non-pressurized cells over the course of 120 hours. Results reported in ESI† show that the pressurization cells indeed allow for acidification of the water they contain, either because they cannot be considered as completely airtight, or because they generate some gas motion accelerating CO2 gas/liquid transfer inside the tubes. The rate at which the pH shifts may depend on the imposed pressure, on the seal model and condition, and on the tightening of the cap, so we did not pursue this issue further. Several solutions are possible to have a good control of the pH for experiments running over a few days: add an inert oil cap above the water in the pressurized tubes, use a CO2 trap before the pressurization system inlet, use nitrogen as pressurizing gas, or use syringe pumps.
In this updated chip design, several modifications have been implemented to facilitate small-angle X-ray scattering (SAXS) measurements on a laboratory beamline. Specifically, the thickness of the OSTEMER walls has been reduced to 50 μm to minimize undesired absorption and scattering. The thickness of the sample-containing channel has been increased to 300 μm to enhance the scattering from the sample, and its width has also been expanded to 300 μm to accommodate the X-ray beam size. Additionally, the channel length has been extended to 3.6 mm, allowing for ten-fold compressions. Because photo-polymerization of a membrane could not be reliably achieved in 300 μm thick channels, a 3D channel design was introduced with the membrane synthesized in a smaller 50 μm high section of the channel.
To evaluate the new design, we performed osmotic compression experiments on Ludox TM50 silica suspensions, which had previously been characterized using standard macroscopic osmotic compression techniques and analyzed with synchrotron radiation. Structural analysis revealed the presence of amorphous phases or mixtures of amorphous and FCC or BCC crystalline phases, aligning with prior observations. These results validate the capability of the setup to establish phase diagrams using a single nanoliter-scale sample, provided the structural transitions are reversible.
The equation of state (EOS) of colloidal suspensions is the other major critical type of data that can be obtained with this setup. We demonstrated that the volume fraction can be tracked over time during compression, either by monitoring X-ray absorbance or by modeling the scattered signals. The former method is universally applicable, even to unknown samples, while the latter requires some prior knowledge of the suspension, such as particle anisotropy or surface reactions. As the osmotic pressure and salt chemical potential are precisely controlled, EOSs can be determined unambiguously from the volume fraction measurements. The shapes of EOSs themselves can already inform qualitatively on phase transitions, offering insights in many practical applications. EOSs can also be compared with existing or new thermodynamic models on more academic topics, such as the determination of effective interaction potentials.
The primary drawback of the present microfluidic chips is their slower compression kinetics, approximately 20 hours per pressure step, compared to the 5–20 minutes per step achieved with chips designed for use under a microscope without simultaneous structure measurements. This difference is due to the increased channel depth and length required for use with a laboratory beamline. When several pressure steps are imposed sequentially, as in this study, continuous measurements over several days require careful pH control in the reservoirs, particularly if pH influences the colloidal suspension being investigated.
This drawback is offset by several significant advantages: (i) the current compression times are still considerably shorter than those required by the traditional osmotic compression technique (1–2 weeks); (ii) most of the benefits of microfluidics, such as small sample volumes and precise control, are retained while offering easier access to laboratory beamlines compared to synchrotron facilities; (iii) the same chip design, but with smaller channels, could be adapted for use with synchrotron sources, enabling compressions on time scales of just a few minutes; (iv) compared to the initial design presented in ref. 24, colloidal particles in the suspension no longer need to be labeled to measure their volume fraction. This is particularly valuable when the surface chemistry of the colloids governs inter-particle interactions, for example in mineral oxide suspensions or dispersions of colloids of biological origin, including proteins and lipid nano-particles.
These microfluidic chips will be valuable for understanding the behavior of colloidal suspensions, particularly when the chemical potential of the small dissolved species, such as ions, needs to be controlled precisely through the membrane. They will find applications in areas such as crystallization, nucleation, soil mechanics, control of living matter growth and interaction conditions, as well as the measurement of coarse-grained colloidal interaction potentials.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4lc01087f |
This journal is © The Royal Society of Chemistry 2025 |