Sebastian
Bindgen
,
Frank
Bossler‡
,
Jens
Allard
and
Erin
Koos
*
KU Leuven, Chemical Engineering Department, Celestijnenlaan 200f, box 2424, 3001 Leuven, Belgium. E-mail: erin.koos@kuleuven.be
First published on 11th August 2020
The structural properties of suspensions and other multiphase systems are vital to overall processability, functionality and acceptance among consumers. Therefore, it is crucial to understand the intrinsic connection between the microstructure of a material and the resulting rheological properties. Here, we demonstrate how the transitions in the microstructural conformations can be quantified and correlated to rheological measurements. We find semi-local parameters from graph theory, the mathematical study of networks, to be useful in linking structure and rheology. Our results, using capillary suspensions as a model system, show that the use of the clustering coefficient, in combination with the coordination number, is able to capture not only the agglomeration of particles, but also measures the formation of groups. These phenomena are tightly connected to the rheological properties. The present sparse networks cannot be described by established techniques such as betweenness centrality.
One hurdle in connecting structure and rheology originates from the presence of the many different length scales that are ubiquitous in the investigated systems. These length scales range from the typical length of interactions far below the particle's diameter, through the cluster scale spanning several particle diameters, to sample spanning scales.1,2 In the presence of attractive particle interactions the stability of larger clusters and connected structures on a more global scale is influenced by the type and strength of the attractive interaction and the ability of particle connections to transmit forces over larger length scales. Rheological phenomena, such as yielding, are influenced by the strength of the attractive interactions as well as the properties of the network such as the dimensionality. This poses a challenge to simultaneously quantify both scales and describe their relative importance.
Multiple tools have been developed to accomplish the task of describing the network structure. A considerable number of these methods rely on image analysis of confocal microscope images.3,4 One key property, often used in particle-based systems, is the coordination number, i.e. the number of contacts that a particle has with its neighbours. For dense systems such as granular matter, the coordination number can be related to mechanical rigidity and the jamming transition.5 In wet granular matter, it has been shown that the mechanical properties of a granular pile increase drastically with the addition of a small amount of liquid forming attractive bridges between neighbouring particles.6,7 The coordination number was also the parameter of choice used by Dibble et al.8 amongst others to describe particle mobility in depletion gels with varying attraction strength as present in less clustered morphologies.9
Besides coordination number, several other network parameters have been investigated. In another depletion gel study, the rigidity of an attractive 3D particle network was characterised using the fractal dimension from image analysis.10 In this work, Dinsmore and Weitz suggested using pivot points and cluster sizes to further characterise different features of the structure. The coordination number was complemented with the void volume fraction to characterise structural heterogeneity in their samples.11 The role of network parameters, such as cycles or centrality measures, in granular matter has recently been extensively reviewed by Papadopoulos et al.5 Two other approaches, using the betweenness centrality in granular matter12 and Cauchy–Born theory in depletion gels,13 are discussed towards the end of our paper.
In short, the need for an easy, rigorous method to connect structure and rheology is only becoming more pressing with improved experimental and computational techniques. In computational experiments, dynamic properties are accessible using improved tracking mechanisms.14,15 Experimentally, a method combining rheology and microscopy and including the measurement of local particle volume fractions was obtained using microrheology.16 Phase separation phenomena and the collapse of structures were also recently investigated.17 The utilisation of knot theory showed the usefulness of mathematical concepts for nematic colloids.18 Nevertheless, finding universal connections between the structure and mechanical properties of suspensions, especially embracing several length scales, remains challenging.
The dimensionality of a network remains a rather arbitrary measure due to the requirement of spacial evenly distributed particle arrangements. Local differences such as dense clusters connected by thin bridges cannot be captured with such a technique and a clear prediction is not possible. The first attempt to successfully predict the modulus of such heterogeneous networks showed that in the region of heterogeneous glasses the modulus is mostly dominated by intercluster contributions to the elastic response where multiple length scales become important.19 Further work elaborated on stable rigid structures present in 2D samples that are dominated by triangles.20
The present study deals with tackling this challenge for the material class of capillary suspensions. Capillary suspensions are created by the addition of a secondary liquid to a two-phase suspension of particles in a bulk fluid, where the secondary and bulk liquids are immiscible.21 These materials are characterised by an overall structure consisting of a percolated network of particles similar to colloidal gels, connected by attractive capillary interactions. While the capillary interactions are the same as in wet granular media, the smaller particle size decreases the Eötvös number, the ratio of gravitational to capillary forces (also called the Bond number), from a value near unity for wet granular media to a value much, much smaller than unity for capillary suspensions.22 This difference in the relative strength of the capillary bridges over the particle weight can be readily observed in the typical solid loading for each system. Wet granular media tends to approach the volume fraction of random loose packing (ϕsolid ≈ 0.5) whereas capillary suspensions tend to have low to intermediate loading (ϕsolid ≈ 0.1–0.4).23 This type of suspensions offers a wide domain of possible applications for the creation of smart materials.24–27
Recent investigations on capillary suspensions have shown a broad range of options to tune the mechanical and rheological properties through changes in their composition,28 which are directly related to changes in their microstructure.22,29,30 Capillary suspensions show, in general, a gel-like behaviour with the storage modulus G′ larger than the loss modulus G′′ and frequency independent behaviour inside of the linear viscoelastic region. Capillary suspensions exhibit a yield stress due to the strong attractive force transmitted by the secondary fluid, even in cases where the particles are not preferentially wetted by the secondary fluid.23 This yield stress shows a non-linear dependence on the amount of secondary fluid, indicating a complex relationship between the network microstructure and the overall network's mechanical response.31 A confocal study has revealed several structural transitions in a silica model system when the wetting behaviour of both liquids on the particle surface is varied.22 The latter was accomplished by modifying the silica beads' chemical surface properties and, therefore, the three-phase contact angle θ, which the secondary fluid forms towards the particles in a bulk liquid environment. In some cases, capillary suspensions can be characterised using scaling concepts that relate rheological data to the fractal dimension.31 This work by Bossler et al. showed a network composed of aggregated flocs and different fractal models provided either the dimensionality of the floc32 or backbone.33,34 These two fractal dimensions become larger with increasing particle size.31 While the fractal dimension can be used to describe the connection between rheology and structure, this method can be problematic for heterogeneous network structures.31 This problem becomes readily apparent in many capillary suspensions.
While electron microscopy images of capillary-suspension-based ceramics microstructures showed structural transitions with different amounts of secondary liquid,29,31,35 no definitive measure exists for the connection between structure and rheology and thus transitions can be difficult to quantify. This is particularly true for the transition from a sparse network towards a more clustered or bicontinuous network for which measures such as the fractal dimension are ill-defined.23,30,36 Therefore, we need an approach that can work equally well for the sparse as well as dense networks. The number of neighbours, the coordination number z, which can be readily calculated from confocal images, provides some insights, but has a tenuous link to rheology. We therefore propose supplementing this measure with another measure from graph theory, namely the clustering coefficient, as shown in Fig. 1. The local clustering coefficient is defined as
(1) |
As illustrated in Fig. 1, intermediate coordination numbers can either have low clustering (c → 0) or high clustering (c → 1) with clear implications of the mechanical response of the cluster. Although the upper limit of the clustering coefficient is c = 1, as shown in the non-physical packed structure in Fig. 1, real, e.g., biological networks, almost never reach this limit and c > 0.5 is considered as high clustering.37
In order to analyse the network properties using graph theory, the 3D particle positions had to be reconstructed as a graph. This was done using the Python package Networkx.43 Each particle was mapped to a node. Node positions were assigned using an individual tag holding their coordinates. These nodes were sequentially connected by edges based on a distance criterion. We chose 6 pixels (0.85 μm) as threshold to detect bonds between individual particles and subsequently to set up edges between graph nodes. For the evaluation of number averages, we ignored particles closer than 2r to the edge of the pictures to ensure that only valid, fully evaluated particles are taken into account. All graphs present mean and standard deviations of the concatenated arrays over all samples.
The result of the graph import procedure was an unweighted graph that was subsequently analysed. We evaluated the coordination number z and clustering coefficient c for each node n.44,45 The number averaged coordination number and clustering coefficient are denoted as and , respectively.
In order to better understand the transitions that occur with added secondary liquid, the sample microstructure is examined using confocal microscopy. Representative 2D slices of one of the eight 3D confocal images, taken for samples with varying ϕsec/ϕsolid for θ = 87° ± 8°, are shown in Fig. 2.
The sample without added secondary fluid (Fig. 2I) does not show a percolating particle network, but rather the structure of a loosely packed sedimented bed. This is easily visible by the much higher apparent solid volume fraction near the slide on the inverted microscope even though the same amount of particles was used during all sample preparations. This implies that any particle interactions are insufficient to overcome the weight of the particles. An addition of only ϕsec/ϕsolid = 0.002 of secondary fluid leads to a completely different structure (Fig. 2II). At such low secondary volume fractions ϕsec, individual particles are connected by binary contacts formed by bridges between asperities. The drops are small enough so that they are not visible in the image due to their size and low dye amount. However, the impact of the drops is clear since the particles form a network with small chains and flocs of particles. These flocs increase in size with increasing volumes of secondary fluid (Fig. 2III and IV). The growth of clusters is linked first to the differing floc growth rate before percolation and second to droplet coalescence. Above a threshold volume, which depends on the contact angle θ, the binary bridges on a particle trimer will touch and merge due to geometrical reasons.22,47 This is the point where aggregates of particles start to form and a funicular state results. For the 87° ± 8° contact angle in these images, this transition is predicted at a bridge volume of Vbridge/Vparticle = 0.03. Assuming a coordination number of 2.5, this transition occurs at a ϕsec/ϕsolid = 0.04 ± 0.02. The merging of the bridges, i.e. a transition from a pendular state with only binary bridges to a funicular state with a clustered structure, is visible in Fig. 2V and VI. Therefore, this transition takes place in the range of 0.038 ± 0.003 ≤ ϕsec/ϕsolid ≤ 0.079 ± 0.003, which correlates very well to the predicted value. The aggregates grow in size and become more dense with further increase in ϕsec/ϕsolid until a bicontinuous structure of particles surrounded by secondary liquid, sometimes called a capillary cluster, is formed (Fig. 2VIII). While the network percolation in this confocal image is no longer visible directly, the large voids of bulk fluid between the particle agglomerates are proof of a stabilisation against sedimentation. This stabilisation is lost with a further increase to ϕsec/ϕsolid = 0.848 ± 0.076 when large, macroscopic agglomerates form (ESI,† Fig. S2). 3D reconstructions of the networks are shown in the ESI,† Fig. S3–S5 where spheres are coloured according to their individual clustering coefficient and coordination number.
The θ = 115° ± 8° samples look similar to the ones with θ = 87° ± 8° at first glance, but they differ in some important ways. First, the sample without added secondary fluid (Fig. 3I) has a solid fraction larger than the average ϕsolid = 0.2, but is less dense than for the lower contact angle. There may be a weak attractive interaction in this sample, meaning that the pure particle interactions in the bulk environment are different between the two contact angles, independent of any additional capillary force. This difference can be fully ascribed to the different surface modifications. While previous experiments have shown that the capillary state is less stable than the pendular state,22 this additional effect may help in supporting the network structure of the θ = 115° ± 8° samples here.
With addition of increasing amounts of secondary fluid, the network formation in these samples is obvious (Fig. 3II–IV). Network formation in the 115° ± 8° sample, however, appears to have a more clustered structure, even at small ϕsec/ϕsolid where individual drops are not visible, e.g. ϕsec/ϕsolid = 0.029 ± 0.007 (Fig. 3III). This means there is no transition from a linear, fractal-like network to a clustered structure, as was the case in the θ = 87° ± 8° sample. In the capillary state samples with θ > 90°, particles should aggregate around small droplets of secondary liquid. There are indeed capillary-state-like microclusters of particles around small droplets visible, as well as singly-connected droplets, which reside on particle surfaces without contributing to the network.22 Previously computational models of capillary state samples predict a transition from tetrahedral to larger particle number clusters with increasing amount of secondary fluid. The shear moduli and yield stress are expected to either reach a constant value or increase slightly in this region.46
Atypical for capillary state samples, however, is the visibility of unexpected binary bridges in Fig. 3V. It is also noteworthy that the particles form bicontinuous aggregates in the worse wetting secondary fluid instead of the better wetting bulk fluid at ϕsec/ϕsolid = 0.451 ± 0.037 and in the phase separated clusters at ϕsec/ϕsolid = 0.737 ± 0.013. These phenomenon may be related to the particle roughness causing a large contact angle hysteresis. 3D reconstructions of the networks are shown in the ESI,† Fig. S6–S8.
The example segments are shown in Fig. 4, where we display a string of particles with small side branches (Fig. 4a), a square backbone arrangement (Fig. 4b), a string of particles with more tightly incorporated side branches (Fig. 4c), and particles with a triangular backbone (Fig. 4d). The square grid arrangements, illustrated in Fig. 4a and b both have = 0 despite the difference in the number of side branches and corresponding . In both cases, there are no triangles formed by bonds between neighbouring particles. These bonds between neighbouring particles, and hence a nonzero clustering coefficient, can be seen in examples Fig. 4c and d. In example Fig. 4c, a structure is introduced with a main path connecting several, more tightly incorporated side beads. Whereas the main path has rather lower clustering, the side beads are fully tight to the graph forming cliques due to the formation of all possible triangles. Example Fig. 4d shows a triangular backbone of particles. Here, an average clustering coefficient of = 0.5 is visible. This threshold is crucial for the later considerations in the histogram, because it allows us to distinguish thicker structures in Fig. 4d from thin structures as formed in Fig. 4c.
Fig. 5 Average coordination number and clustering coefficient for θ = 87° ± 8°. The roman numerals correspond to the images shown in Fig. 2. |
A more detailed view on the first five points in this graph is shown in the ESI,† Fig. S9.
While the average values give some indication for the changes in the network structure, key transitions can be hidden by subtle changes in the average values. The histograms of all samples are therefore shown in Fig. 6.
Fig. 6 Histograms of the coordination number and clustering coefficient for all samples with a contact angle of θ = 87° ± 8° for several amounts of secondary fluid. |
These histograms will be used to show key transitions in the microstructure and finally to tie these changes to the resulting rheological properties. For all histograms, the clustering coefficient is shown in green and the coordination number in blue. All shown histograms are normalised so that the integral value over all bins is 1. A comparison between low (c ≤ 0.2), medium (0.2 ≤ c < 0.4), high (0.4 ≤ c < 0.6) as well as the remaining (0.6 ≤ c) clustering coefficient is shown in Fig. S10 (ESI†).
We will first consider the sample that corresponds to the pendular state samples (θ = 87° ± 8°). A broad distribution of coordination numbers can be seen for the sample without added secondary liquid (Fig. 6I) with a mean value of = 5.1. The mean value of the clustering coefficient is = 0.15. A lot of particles with a clustering coefficient around the theoretical minimum of c = 0 can be observed, indicating particles without tight clustering. These values are characteristic for a loosely packed sedimented bed. That means there is a random arrangement of particles present where polydispersity of the particles can lead to a lot of isolated particles or particles with only one neighbour. This low clustering can indicate a metastable structure.48 Indeed, the structure of this sample changed slightly during the measurements, either due to the small movements of the objective or very slow sedimentation.
With the addition of secondary fluid to ϕsec/ϕsolid = 0.002 ± 0.001 (point II), we can see the structural arrangements due to the filling of the particles asperities in the histograms. Particles are connected to each other via binary bridges leading to a lower average contact number of = 3.1 while the average clustering coefficient rises to = 0.19. This rise is caused by two effects. First, a number of particles with a high clustering coefficient close to c = 1 appears. These highly clustered particles are arrangements of trimers or other small groups of particles, often located on the outside of flocs or strands. Second, a new peak emerges at an intermediate value of the clustering coefficient around c = 0.3, which is consistent with particles in a partially reinforced backbone chain as illustrated by Fig. 4b. However, one must not ignore the rise in the amount of particles having low or zero clustering. We conclude from the corresponding histogram of the coordination number that there is a change from the random sediment arrangement into an open network with many short, linear branches of two or three, as indicated by the increase of particles with coordination number z = 1 to z = 3.
The same trend continues at ϕsec/ϕsolid = 0.011 ± 0.001 (Fig. 2III), where a fractal-like gel structure is visible. The average coordination number once more lowers to about = 2.7. Furthermore, the amount of particles with a coordination number of z = 2 reaches its global maximum compared with the other histograms. The distribution of the clustering coefficient, which has an average of = 0.15, shows the same features as above but is even more pronounced. As the number of particles with low clustering coefficient rises, more binary contacts are present. This rise is associated with a decrease in the number of particles with intermediate clustering, indicating a change towards the linear branched structure of Fig. 4a. The amount of particles at the maximum clustering coefficient shows no change (see also Fig. S2, ESI†). Such a transition would be consistent with the formation of a weak gel structure dominated by binary contacts (Fig. 4a) and some tightly arranged clusters formed by trimers or other low number particle groups (Fig. 4b).
As the structure changes towards a funicular, or clustered, state (Fig. 2IV), the coordination number increases to a value of = 3.5. The average clustering coefficient also increases to = 0.21, but the change in the average, shown in Fig. 5, is quite modest. The histogram shows a clearer loss in the number of particles with very low clustering and an increase in the intermediate clustering. We believe that this is caused by the addition of particles to already existing clusters, leading to their increase in size and not by the formation of entirely new groups of particles. This funicular state is akin to the sketch in Fig. 4b with the size of the triangular (or, in 3D, tetrahedral) clusters growing in size.
With the next three additions of secondary liquid, corresponding to the growth of funicular clusters and the transition to a fully bicontinuous structure, the average coordination number has values of = 4.1, = 4.9 and = 4.6, respectively. The clustering coefficient approaches a plateau with average values of = 0.26, = 0.38 and = 0.39. These are values that are typical of small-world phenomena in graph theory. Small world graphs have nodes that are not direct neighbours (low z or degree) but are only separated from each other by a few hops (a few particles). Put another way, these graphs are composed of tight cliques with few connections between cliques. These maximal cliques are defined as groups of nodes (particles) where every two nodes are adjacent (forming a triangle) and the number of triangles would not be increased by including more nodes. Thus, the cliques are tight flocs of particles with few inter-floc connections. A look at the confocal images reveals the presence of particle groups that become more and more isolated, indeed forming the small interconnected worlds. The confocal picture with ϕsec/ϕsolid = 0.418 ± 0.036 (Fig. 2VIII) especially illustrates that state.
With the final addition of secondary fluid, the structure phase separates. This is indicated by the clustering coefficient decreasing to an average value of = 0.25, towards the initial sedimented bed state. However, the structure seems to be denser than the initial sediment, as shown by the increased clustering coefficient and coordination number ( = 7.2). This can be explained by the fact that the secondary liquid is solely present between the sedimented particles, pulling them together more tightly. This means that the arrangement of particles is not as loosely arranged as in the first state without secondary liquid added. This structure should be more resilient to external deformation.
The average values for the θ = 115° ± 8° series of samples, i.e. the capillary state system, are shown in Fig. 7 and histograms of coordination number and clustering coefficient are shown in Fig. 8.
Fig. 7 Average coordination number and clustering coefficient for θ = 115° ± 8°. The roman numeral correspond to the images shown in Fig. 3. |
Fig. 8 Histograms of the coordination number and clustering coefficient for all samples with a contact angle of θ = 115° ± 8° for several amounts of secondary fluid. |
The average coordination number for the sedimented bed = 3.3 is a lower than for the pendular state samples and the clustering coefficient, has the same average value of = 0.15. The histograms for this first θ = 115° ± 8° point (Fig. 8b(I)) resembles that of the θ = 87° ± 8° sample with wetted asperities (ϕsec/ϕsolid = 0.002 ± 0.001, Fig. 6II).
Interestingly, the development of a network in the capillary state seems to follow a different pattern than in the pendular state. Instead of an increasing amount of particles with clustering coefficient near zero, i.e. binary contacts, one can see that the amount of such particles is reduced in this sample. Instead, there is a large percentage of particles with intermediate or high clustering. The distribution between the clustering coefficient ranges is again shown in Fig. S10 of the ESI.† With the addition of secondary fluid, the average coordination number and average clustering coefficient both rise. This is consistent with both computational models of the capillary state where particles surround small fluid droplets forming polytetrahedrons15,23 and is also consistent with the confocal images (Fig. 3) showing particle clusters.
The histograms reveal that even with small amounts of secondary liquid, the overall distribution of the coordination number is broader compared to the pendular state samples. Furthermore, the peak at c = 0.3 is much more pronounced in early stages of the network buildup. Together with the lower amount of particles at c = 0, we conclude that much fewer binary contacts are present. Overall, the histograms do not change much with the addition of secondary liquid, although the averages increase slightly, indicating that structures present in the sample are growing while the inner arrangement of the structures themselves remains unaltered and does not undergo significant phase changes.
A special effect can be seen between ϕsec/ϕsolid = 0.193 ± 0.009 (Fig. 3VII) and ϕsec/ϕsolid = 0.451 ± 0.037 (Fig. 3VIII). Between these points, the network transitions from a network of small clusters with many connections to a bicontinuous structure with large clusters and few connections. Between these two points, the average clustering coefficient remains unchanged, but there is a shift from low clustering (c ≤ 0.2) to medium clustering (0.2 < c ≤ 0.4) as shown in Fig. S3 (ESI†). There is also an increase in the average coordination number from = 5.4 to = 6.2, driven by a nearly uniform shift in the histogram to the right.
As with the pendular state samples, phase separation takes place at high ϕsec/ϕsolid in the capillary state system. The coordination number reaches a maximum of = 7.6 and the clustering coefficient returns to a value of = 0.26. Both the shape of the histograms and the average values indicate that this separated state is essentially the same between the pendular and the capillary state samples.
(2) |
A steep increase in the suspension's strength occurs for low amounts of ϕsec/ϕsolid. Both G0′ and G′′(γcrit) show a maximum at an intermediate amount of added secondary fluid, albeit at slightly different ϕsec/ϕsolid values. After this maximum, the network strength begins to decrease again. This behaviour is characteristic for pendular state samples.29,31,50 As was previously hypothesised and confirmed with confocal images,22,46 the stress increase at relatively low amounts of secondary fluid should appear due to the buildup of binary capillary bridges, where the maximum is attributed to a coalescence of adjacent bridges, termed the funicular state. The decrease for relatively high amounts of secondary fluid is explained by the formation of large and dense particle agglomerates (e.g.Fig. 2VIII) that begin to destabilise the structure.29,31
Of particular interest in the pendular state is the transition to the funicular state, which should correspond to the maximum stress values in the rheological data of Fig. 9 in the range of 0.038 ± 0.003 ≤ ϕsec/ϕsolid ≤ 0.079 ± 0.003. This value also coincides with a transition from binary bridges to a clustered structure shown in (Fig. 2V and VI). Thus, the decrease in strength observed in the rheological data indeed correlates to the formation of large agglomerates which would reduce the number of network contacts. Point VI also corresponds to the end of the rapid rise region in and . Points V and VI show a slight broadening of the coordination number histogram and a clear decrease in the number of particles with low or zero clustering and an increase in the particle fraction with intermediate or high clustering. Indeed, this metric shows that the clustering actually begins earlier – at point IV, ϕsec/ϕsolid = 0.018 ± 0.002 – when the fraction of particles with c = 0 begins to decrease. This may not be manifested in the shear moduli due to the small fraction of clustered particles, but may effect other rheological measures such as yielding.
Contacts alone, however, are insufficient to create a high elastic modulus. In capillary suspensions with hard spheres, momentum transport contributing to the elastic response has to originate from the secondary liquid. Without secondary liquid, there might be a lot of particle contacts, but these particle contacts rely solely on friction to transmit momentum. Friction forces mostly act perpendicular to the position vector connecting the particles centres via their contact point and, thus, do not contribute to the off-diagonal elements i.e. the shear stress. Adding secondary liquid to fill the particles' asperities makes these contacts effective for the transmission of normal forces. Thus, the modulus of the samples begins to increase despite the average coordination number being lower than the one measured in the sedimented bed state. Increasing the amount of secondary liquid beyond the point of filled asperities decreases the average coordination number and seems to contradict our hypothesis at first sight. However, the lowering of this average coordination number is mostly caused by the vanishing number of particles with a high contact number and not by a shift in the entire distribution (Fig. 6). Furthermore, samples with a z = 4 (point V) fulfil the condition of isostaticity for spheres with friction which can explain the steep rise in moduli as well.52,53
The relationship between an increasing number of bonds increasing the transmission of momentum in the sample holds true through the peak G0′ until point VII (ϕsec/ϕsolid = 0.165 ± 0.016) as shown in the ESI,† Fig. S11. Here, an interesting effect can be observed. First, the average coordination number decreases. However, the average clustering coefficient continues to increase. That means more closed aggregates are formed. These closed aggregates are analogous to the cliques in a small world network. These local clusters redistribute energy inside themselves, as previous works of graph theory have shown.54 The clusters distribute the motion between their many contacts, rearranging the structure and dissipating any motion. The energy, thus, becomes unavailable. This unavailable energy leads to a drop in the modulus that is not compensated for by the subsequent rise in the coordination number. This is due to the fact that these aggregates become more and more cliquish with high internal interconnectivity, but few contacts bridging the flocs. As already mentioned in the introduction we expect the physical networks to not show an overall clustering coefficient of = 1 due to restraints of spatial embeddedness. However, it seems evident that the movement of one particle in such an arrangement can influence the movement of all other particles that are part of the same local cluster. This corresponds to the concept of a clique that connects beyond spatial embeddedness. Similar results have already been observed in optical tweezer experiments. Here, a transition from a cluster-like to a string-like gel was observed indicating a decrease in the long-range structural heterogeneity along with the occurrence of anomalous strain fields.55 At the last point, the clustering coefficient decreases with the moduli, which has been previously reported to be an indication for material failure, or in the case here, phase separation.5
In analogy to the elastic response, we can tie the initial rise in the viscous stresses to the fact that structure formation yields a state where many individual particles are surrounded by bulk fluid increasing the external surface area. This increases both the amount of fluid participating in the friction effects on the surface of particles and the amount of primary liquid in the void between the particles, generating stress. This effect seems to cause a rise in the viscous modulus proportional to the rise in the storage modulus for the low amounts of added secondary fluid before point III (ϕsec/ϕsolid = 0.011 ± 0.001). However, the loss and storage moduli reach their maxima at point V (ϕsec/ϕsolid = 0.038 ± 0.003) and point VI (ϕsec/ϕsolid = 0.079 ± 0.003), respectively. We believe this to be an indication of the pendular–funicular transition that means the merging of binary bridges of secondary liquid to larger interconnected structures. This process decreases the fraction of particles with c = 0, leaving only particles of higher clustering with the most prominent peak at c = 0.3. The formation of larger and larger clusters continues to decrease the surface area, causing the drop in skin friction and G′′ in the system. This pendular to funicular transition is marked by a change from a positive correlation between the structure parameters and dynamic moduli to a negative correlation, as shown in Fig. S11 (ESI†).
Again, the phase separated samples (points I and IX) are not shown. Unlike for the pendular state sample, the capillary state does not exhibit a pendular–funicular transition or any other characteristic transitions with the exception of the highest and lowest ϕsec/ϕsolid (not shown). Instead, a gradual increase of the storage and loss moduli is observed in the rheological data of Fig. 10, where also no maxima or other hints for clear transitions were observed. This finding fits very well with the more gradual structural changes, which mostly just show an increasing size of bridges and droplets with increasing secondary fluid volume.
The connection between the sample microstructure and the resulting rheological properties in the capillary state resides on the same foundation as the pendular state, regardless of the difference in contact angle. Indeed, we can again observe a direct correlation between the main coordination number, the clustering coefficient and the presented moduli. Even the structural transition between ϕsec/ϕsolid = 0.088 ± 0.006 (point V) and ϕsec/ϕsolid = 0.192 ± 0.006 (point VI) is well reflected in the rheological as well as the structural data (see Fig. S11, ESI†). As the overall ratio between and does not change with the addition of secondary liquid, we would not expect sudden changes in the moduli. This is indeed the case here. Only upon phase transition at the very end an extreme change in the structure parameters can be observed. Previous comparisons between samples showed that the elastic modulus or yield stress was lower in capillary state samples compared to the pendular state.31 We would argue that this difference can arise from the differences in the cliquishness alone, and thus, these measures may not indicate differences in bridge strength. Indeed, in the present samples, the pendular samples with low amounts of ϕsec/ϕsolid (lower coordination number ) are weaker than in the capillary state and the bicontinuous samples have nearly identical structural parameters and moduli.
A further example is the study of depletion interaction gels.13 In this work, Whitaker et al., studied the structure and rheology of depletion interaction gels with varying attractive potential. The contact number of particles was investigated the same way presented here. However, the mean and width of the coordination number distribution only changed slightly upon an increase of the attractive strength. While not explicitly measured, there is also likely less variation in the clustering coefficient since the internal volume fractions of the cluster only varied from 0.3 to 0.35. Capillary suspensions offer much more versatility as a model system due to the possibility to actively tune the amount of particle neighbours via the amount of secondary liquid added and the mixing conditions. The approach of l-balanced graph partition offers great possibilities for capillary suspensions, e.g., in the regions of high secondary volume fractions. It comes, however, with the caveat that the amount of particles in the such a decomposition has to be chosen. Especially in the region of linear arrangements, where not a lot of pronounced particles groups are present, this choice remains rather arbitrary. Furthermore, it introduces a further step in the processing, that is not necessary when, e.g., the clustering coefficient is used. Perhaps, however, the combination of the two methods can be used to expand the robustness and insights provided by each method.
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/d0sm00861c |
‡ Present address: Zeppelinstraße 1c, 85375 Neufahrn, Germany. |
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