X-ray 3D imaging–based microunderstanding of granular mixtures: Stiffness enhancement by adding small fractions of soft particles
Edited by David Weitz, Harvard University, Cambridge, MA; received November 23, 2022; accepted May 21, 2023
Significance
The focus is on structure–property relations of biphasic granular mixtures composed of soft and stiff particles subjected to a range of uniaxial stress conditions. Ultrasonic experiments have shown that for an optimal number of soft inclusions, one can observe material properties different from the mere superposition of ingredients. The impact of particle arrangements, subnetworks, and force chains on the mechanical response of soft-stiff granular compositions is deduced from in situ micro-X-ray computed tomography measurements. Identifying shorter chains of stiff particles at the microscale explains one possible cause behind the stiffening of samples. This interesting nonlinear and nonmonotonic transition from stiff- to soft-controlled media is described by the jamming of subnetworks, which might be useful for the design of materials.
Abstract
This research focuses on performing ultrasound propagation measurements and micro-X-ray computed tomography (µXRCT) imaging on prestressed granular packings prepared with biphasic mixtures of monodisperse glass and rubber particles at different compositions/fractions. Ultrasound experiments employing piezoelectric transducers, mounted in an oedometric cell (complementing earlier triaxial cell experiments), are used to excite and detect longitudinal ultrasound waves through randomly prepared mixtures of monodisperse stiff/soft particles. While the fraction of the soft particles is increasing linearly from zero, the effective macroscopic stiffness of the granular packings transits nonlinearly and nonmonotonically toward the soft limit, remarkably via an interesting stiffer regime for small rubber fractions between 0.1 ≲ ν ≲ 0.2. The contact network of dense packings, as accessed from µXRCT, plays a key role in understanding this phenomenon, considering the structure of the network, the chain length, the grain contacts, and the particle coordination. While the maximum stiffness is due to surprisingly shortened chains, the sudden drop in elastic stiffness of the mixture packings, at ν ≈ 0.4, is associated with chains of particles that include both glass and rubber particles (soft chains); for ν ≲ 0.3, the dominant chains include only glass particles (hard chains). At the drop, ν ≈ 0.4, the coordination number of glass and rubber networks is approximately four and three, respectively, i.e., neither of the networks are jammed, and the chains need to include particles from another species to propagate information.
Sign up for PNAS alerts.
Get alerts for new articles, or get an alert when an article is cited.
Granular matter has an intrinsic heterogeneous nature; this is expressed, for instance, in discrete force chains developed between the grains within the granular medium. Force chains spread the forces inhomogeneously through the contacts with neighboring particles (1–3). Interactions of particles cause strongly different force magnitudes on close particles and dependent on the boundary condition, nonisotropic stress throughout the medium. Force chains are due to disorder but also depend on small-scale properties like the local stress state, surface roughness of the individual grains, size distribution, particle shape, packing fraction, and interparticle friction. The heterogeneity is manifest in the fact that granular matter exhibits a strong configuration and history dependence, well known for decades in industrial applications and fields like soil mechanics (4).
Noise and vibration constitute a drawback in many technical and geoengineering applications. Acoustic waves produced on roads, railways, or by earthquakes propagate through granular materials (like soil, gravel, or asphalt), with the characteristics of the aggregate affecting the overall response. Mechanical waves are perturbations moving through space and time in a medium where small-enough deformations lead to elastic restoring forces. This produces a transfer of momentum and/or energy from one point to another, usually involving little or no associated mass transport (5–7). Probing a material with (ultra) sound waves can give useful information on its state, structure, and mechanical properties.
The P-wave, or primary wave (also named longitudinal or compressional), exists in solids and fluids—unlike the secondary or S-waves (shear or transversal) that propagate in solid media only (8). The P-wave is the fastest and the first signal detected by seismographs when traveling through the earth’s crust. In a P-wave, particle displacements are longitudinal, parallel to the direction of wave propagation, whereas in an S-wave, displacements are perpendicular (9).
The propagation of elastic waves, such as P-waves, is a nondestructive testing method. It involves small perturbations that do not alter the microstructure or cause permanent effects. When the wavelength is significantly longer than the internal scales of granular packings, such as particle or cluster size, the propagation velocity can be defined for the equivalent continuum, where the elastic moduli and mass density refer to the bulk medium (10). Small-strain stiffness, i.e., elastic stiffness, is a fundamental macroscale mechanical parameter for a wide range of engineering problems, and it is used for the prediction of granular response under both static and dynamic loading conditions (11–18). If both conditions, small amplitude and long wavelength, are fulfilled, wave measurements can be used to infer elastic stiffness (19–22).
The composition of granular materials can vary widely, and while some granular systems may consist of differently sized and shaped particles with similar properties, others are mixtures composed of particles with different properties (hundreds in some industrial processes or in natural soil). Nevertheless, their multispecies mechanisms and mixture bulk properties are far from being understood—even for the simplest case of two components. The properties of aggregates made of stiff and soft beads have been extensively studied experimentally (23–29) and numerically (30–38), varying the rubber content and the confining stress. Recent studies have shown that granular mixtures can have a surprisingly large elastic stiffness but are lighter and more dissipative thanks to the soft particles (39, 40). Mixtures with a small number of soft particles propagate sound faster than material made by stiff particles only (24, 39, 40). However, the nature of this phenomenon has yet remained open, for which we extract and investigate deeper the available microinformation of samples.
Earlier investigations have shown the importance of particles’ networks, in controlling the effective mechanical properties of particulate systems on larger scales, e.g., elastic moduli (41–47). The particle–particle contacts support large forces are usually correlated in a linelike fashion (though they are not completely linear) over distances of several particle diameters, leading to so-called force chains (48–51), i.e., a contact transmitting a force is balanced with a single contact on the opposite side of the grain, and this is repeated on several subsequent grains (22).
In static equilibrium, force chains play a crucial role in transmitting acoustic waves, eventually, the stiffness of the granular packings. Although wave propagation is a promising technique to acquire the small strain stiffness of granular packing, it is unable to reveal crucial microstructural details. The use of micro-X-ray computed tomography (µXRCT) has allowed for unprecedented observations, such as fabric evolution, strain localization, deformation and failure, fracture and fragmentation, segregation, and jamming (52–56) and a renewed understanding of particulate systems by offering a possibility to visualize the internal discrete structure of the media (45, 57–62). Its advantage to provide a representation of particulate systems has led to gaining extensive information down to the scale of single particles (63).
In this study, we apply µXRCT-based characterization to provide access to the discrete microstructure for biphasic packings of glass and rubber particles. The stress state of the sample is controlled by an applied uniaxial compression state. By combining high-resolution µXRCT characterization containing microscale logical information with macroscale ultrasound propagation measurements, we explain the role of particles’ contact networks on the effective macroscopic mechanical response of granular mixtures. In a nutshell, this research provides insight into features of wave propagation in randomly packed stiff–soft mixtures to enlighten the fundamental mechanisms controlling small-strain bulk stiffness in such systems.
Results and Discussion
Small-Strain Stiffness.
To obtain the P-wave modulus of the biphasic sample, M, the ultrasound velocity (Vp = Lz/tp) is measured knowing the travel time of the wave into the sample (tp) and the sample height after deformation (Lz). The bulk density of the sample is determined for different rubber fractions as ρ0 = ν ρg0 + (1 − ν) ρr0, where ρg0 and ρr0 are the glass and rubber densities (ρg0 = 1,540 kg m−3 and ρr0 = 860 kg m−3 (40)) at preparation (p = 0), and ν is the rubber fraction of samples ν = Vr0/V0, where Vr0 and V0 are the volume occupied by the rubber beads and the volume occupied by all particles (V0 = Vr0 + Vg0), respectively. Thanks to the calculated mass density, ρ0, of the sample, and the experimentally obtained wave velocity, the longitudinal P-wave modulus is being determined by M = ρVp2 = ρ0(Lz0/Lz)Vp2.
Fig. 1 illustrates the relationship between the small-strain stiffness, denoted as M, and the five vertical stresses, p, which are the resultant of the applied axial stress for samples with varying fractions of soft/stiff particles. Each experiment was repeated five times for every rubber content to obtain new configurations (i.e., new particle arrangements). The SD of the modulus is included in Fig. 1 for p= 80 kPa and 160 kPa with vertical bars.
Fig. 1.

As the applied vertical stress on the sample increases, its porosity decreases, making it denser and resulting in an increase in stiffness. Fig. 1 shows three different regimes highlighted in different colors as we move along the x-axis: i) Up to ν ≈ 0.3, the response is mainly controlled by stiff particles (red color in the background of Fig. 1). The tests conducted under uniaxial compression using an oedometer cell show a slight increase in the P-wave modulus, upon adding a small fraction of rubber particles; ii) adding more rubber beads leads to a drop of modulus for 0.4 ≲ ν ≲ 0.6. This indicates that the samples are weakened, as shown by the cyan color background in Fig. 1; iii) rubber occupies most of the total volume for ν ≳ 0.6 where the sample is fully controlled by soft particles. Thus, the stiffness remains constant even with the addition of more rubber particles (highlighted by the yellow color background in Fig. 1). This is due to the softness of rubber particles, which can deform significantly, leading to surface contacts instead of point-to-point contacts between particles. These samples are more like a porous rubber media with glass inclusions, and the packing seemingly resembles that of an inhomogeneous rubber block (64, 65). It must be noted that the maximum deformation applied to the samples (especially soft samples) is 10% of the initial sample height (Lz0= 80 mm), which is within the elastic limit of the rubber particles, so they do not deform permanently (30).
The oedometric cell experiment under uniaxial compression with zero lateral strains supports earlier research conducted by the authors using triaxial cells with isotropic stress control (40). However, it is still unclear how rubber strengthens samples for ν = 0.1 and 0.2. The microstructural mechanisms responsible for the transition from stiff- to soft-dominated networks have yet to be resolved. Therefore, we employ in situ µXRCT to provide a microinvestigation at the particle scale. Another representation of the modulus plotted against the applied stress is shown in SI Appendix, Fig. S1. In addition to the wave propagation tests performed under the stress-control condition, we performed complementary tests following a strain-control protocol for samples ν = 0, 0.1, 0.2, and 0.3, which is given in SI Appendix, Fig. S2.
Particles’ Contact Network.
Mechanical response investigations of samples using (ultrasound) wave propagation have allowed identifying the most interesting regime (0.1 ≲ ν ≲ 0.6) for in situ µXRCT experiments. The particles’ contact networks of some samples are studied next using the extracted information such as particles’ centroid and their contact locations with one another. To begin with, we classify particles according to the number of particles they are connected to. In Fig. 2A, we can see the distribution of particles based on the number of contacts they have. The y-axis (Np) represents the number of particles, while the x-axis (c) shows the number of contacts within the respective subnetworks. These results are based on images obtained at p = 160 kPa and different rubber fractions ranging from 0.1 to 0.6. SI Appendix, Fig. S3 displays the analysis carried out on images collected at p = 80 kPa.
Fig. 2.

At first glance, all-network data appear to follow a Gaussian distribution function, as shown in Eq. 1. The function provides histograms that represent the number of particles based on the number of contacts they have:
[1]
In Eq. 1, c is the number of contacts carried per particle, a is a fitting parameter, σ is the SD with respect to the mean, and is the coordination number of a sample, which is defined by
[2]
Dashed and solid black lines are the fitted plots using Eq. 1 for samples with ν = 0.1 and 0.6 scanned at p = 160 kPa, respectively. The distribution of particles and their contacts indicates that the samples almost coincide on the same function, regardless of particle characteristics. However, when more rubber particles are added (ν ≳ 0.4), the plots shift slightly to the right, due to the nature of rubber particles, which can deform and create more contacts with neighboring particles.
Next, the networks are split into glass (G–G, Fig. 2B) and rubber (R–R, Fig. 2C) subnetworks for each sample, where only particles belonging to a single species are taken into account. For completeness, we plot in SI Appendix, Fig. S4, the connectivity of glass and rubber where only the contacts between rubber and glass particles are considered and not the ones from the glass–glass and rubber–rubber subnetworks. Both Np and c decrease as ν increases. On the contrary, the opposite trend is observed in the rubber subnetwork plots. Comparing the data of ν = 0.1 (red) and ν = 0.2 (blue), the number of particles with a high number of contacts is quite similar in the glass networks, i.e., the right tail of the glass network is very similar for both cases. In contrast, this is not observed for rubber networks where almost all rubber particles carry just less than three contacts for ν = 0.1.
Earlier studies have shown that particles carrying less than three contacts, so-called rattlers, are not mechanically stable and do not contribute to force networks since their few contacts are momentary (66–69). The networks that are considered in this study exist in a dense regime under gravity, and as a result, there are very few rattlers. This can be observed in Fig. 2A, where the plot shows that only a small number of particles (Np) have less than four contacts (c). However, when considering only a rubber network with ν ≈ 0.1, the isolated clusters of rubber particles exhibit similar characteristics to rattlers in a loose packing. This is due to the fact that rubber has a stiffness that is three orders of magnitude smaller than that of glass, and as a result, rubber particles surrounded by glass, similar to an isolated “void,” do not contribute significantly to the force network in comparison to glass–glass contacts. Therefore, the overall response of the entire network is controlled by the glass particles. The main difference between a sample with ν = 0.1 and a pure glass sample is the deformability of the bulk due to the rubber islands, which reduces the length of the sample.
In contrast, samples with ν ≳ 0.2 contain more rubber particles with coordination above three. Some of these particles participate in the overall force networks by forming chains, loops, or clusters between themselves and glass particles, but the amount of rubber particles is yet not sufficient to influence the overall network. The sample with ν = 0.3 shows a qualitatively similar response as ν = 0.2. Nevertheless, the overall response of the network is weaker since stiff particles are replaced by soft ones, which leads to a decrease in M-modulus when ν ≳ 0.3.
Finally, to illustrate the evolution of networks, glass and rubber subnetworks are shown in Fig. 3 for two samples, ν = 0.1 (A and B) and ν = 0.5 (C and D), compressed under p = 160 kPa. Comparing (B) and (D) subfigures (rubber network), we observe many isolated rubber particles with almost zero or one contact which cannot form a chain/path for wave propagation. In contrast, a highly dense network has formed for the rubber network of ν = 0.5 in subfigure (D), indicating an increase in the coordination number and demonstrating the transition from a stiff- to soft-regime.
Fig. 3.

The next microparameter investigated here is the coordination number, Eq. 2, which reveals more quantitative information about the microstructure. In Fig. 4, we demonstrate the evolution of the coordination number, , of glass subnetwork, rubber subnetwork, and overall networks for samples with different rubber fractions at p = 160 kPa. If we take into account all the particles in the networks, we can observe that the coordination number (indicated by the green line) increases slightly as the rubber content increases. This is because the rubber particles are more deformable, which leads to the formation of more contacts between all particles due to the lower bulk volume. As rubber content increases, the glass subnetwork deteriorates further while the rubber–rubber network develops.
Fig. 4.

Earlier studies have shown that if the coordination number of a system under compression exceeds a certain value, it enters a regime known as a “jammed” state, where contacts are permanently established (3, 68–71). At jamming, where the system transits from liquid-like to solid-like state, the system becomes mechanically stable with finite bulk and shear moduli. Different parameters influence the coordination number. Higher friction lowers the coordination number ( 5.5 for friction equal to one; dashed line in Fig. 4), while lowering friction increases both the coordination number ( 6 for frictionless particles) and the volume fraction of jamming (72, 73).
One key observation one can make from comparing the coordination numbers of subnetworks of samples with rubber fractions ν = 0.1, 0.2, and 0.3 is whether each of the subnetworks is in a jammed state or not. The coordination numbers of the glass–glass subnetworks of samples with rubber fractions ν = 0.1 and 0.2 are above 5.5, confirming that these networks are surely jammed. This indicates that the glass subnetworks of ν = 0.1 and 0.2 are in a stable state with a finite stiffness not requiring rubber particles. However, the coordination number of the glass–glass subnetwork of the sample with a rubber fraction of ν = 0.3 is close to five, slightly below the jammed state coordination. Therefore, to reach a mechanical equilibrium with a finite stiffness, the glass–glass subnetwork relies on the rubber particles for ν ≳ 0.3.
Incorporating rubber particles—although it increases the coordination number and eventually offers a jammed packing—the overall stiffness of the packing starts to decay due to the softness of rubber. This explains the nonlinear, nonmonotonic behavior of the M-modulus observed in Fig. 1 for low rubber content samples. The presence of more and more rubber particles for ν = 0.1 and 0.2 makes the samples more deformable than an only glass sample, ν = 0, and the sample with ν = 0.2 is also more deformed in height than the sample with ν = 0.1, as we can see from SI Appendix, Fig. S2A.
Moving along the x-axis of Fig. 1, a further decline in the stiffness occurs at rubber fractions greater than 0.3. This decrease is associated with the change of contact networks from a stiff- to soft-dominated network (40). The regime 0.3 ≲ ν ≲ 0.5 in Fig. 4 is where the phase change starts since both glass and rubber networks carry almost the same coordination number. For rubber fractions greater than or equal to 0.5, the overall network behavior, such as stiffness, is fully controlled by soft particles, as their networks have gained a higher coordination number than that of stiff networks.
Contact Network Morphology.
Previous observations (74) indicated that acoustical waves traveling through the granular medium are transmitted by strong force chains. Thanks to µXRCT imaging (61, 75–77), we are able to extract detailed information about the force chains of mixtures to explain the percolation chains of granular mixtures by postulating that the wave travels along the stiffest (fastest) path.
As earlier studies have shown, see refs. 39 and 40 and Fig. 1, increasing pressure leads to an increase in wave velocity and modulus. When a soft particle comes in between hard particles, due to its softness and viscoelastic features, it dissipates more energy, which leads to slower wave travel. If two identified chains have a similar length, the one which is only made of stiff particles is preferred by the wave to travel faster.
From top to bottom of the samples, a number of chains can be identified. Among possible paths for every sample, depending on selection criteria, the shortest length (the most linear-like) is selected as the fastest propagating path. Fig. 5 demonstrates the packings including one of the identified short chains, where red and blue particles represent glass and rubber particles. To identify the shortest possible chains, the following steps are taken: i) The first layer of particles on top of the samples is identified; ii) for each individual particle in this layer, the neighboring particles are determined. Two particles are considered neighbors if the distance between their centers is equal or less than the diameter of the particles (4 mm); iii) among the neighboring particles, the one with the smallest vertical coordinate (z-direction) is selected; iv) steps (ii) and (iii) are repeated until the last particle of the chain is found at the bottom of the sample. To have a comparison among the identified chains, their lengths are divided/scaled by the sample heights (almost identical in all cases, Lz0 = 80 mm). Table 1 reports the normalized average length of the first ten identified short chains (), their SD, number of particles involved in the chains (), and the shortest path among all the ten identified chains (ℒ). As mentioned earlier, we have repeated µXRCT two more times for samples prepared with ν = 0.1, 0.2, 0.3 with new configurations by removing and adding the particles for every test. The statistical characteristics of these tests are also included in Table 1 for completeness.
Fig. 5.

Table 1.
ν | Sample | SD | min(ℒ) | ||
---|---|---|---|---|---|
0.1 | 1 | 1.3221 | 0.0215 | 24 | 1.2917 |
2 | 1.3114 | 0.0323 | 24 | 1.2405 | |
3 | 1.3126 | 0.0497 | 25 | 1.1839 | |
0.1 | Mean ± SD | 1.3154 ± 0.0048 | 0.0345 ± 0.0116 | 24.3333 ± 0.4714 | 1.2387 ± 0.0440 |
0.2 | 1 | 1.2536 | 0.0438 | 23 | 1.1916 |
2 | 1.2536 | 0.0411 | 23 | 1.1816 | |
3 | 1.3259 | 0.0296 | 24 | 1.2055 | |
0.2 | Mean ± SD | 1.2777 ± 0.0341 | 0.0382 ± 0.0062 | 23.3333 ± 0.4714 | 1.1929 ± 0.0098 |
0.3 | 1 | 1.3367 | 0.0340 | 24 | 1.2886 |
2 | 1.3231 | 0.0371 | 24 | 1.2370 | |
3 | 1.3350 | 0.0357 | 24 | 1.2914 | |
0.3 | Mean ± SD | 1.3316 ± 0.0061 | 0.0356 ± 0.0013 | 24.0000 ± 0.0000 | 1.2723 ± 0.0250 |
0.4 | 1 | 1.3563 | 0.0405 | 25 | 1.29902 |
0.5 | 1 | 1.3443 | 0.0284 | 26 | 1.30419 |
0.6 | 1 | 1.3501 | 0.0317 | 25 | 1.30524 |
From Fig. 4, we learned that the sudden drop of modulus for samples with ν ≳ 0.4 is due to a change of networks. The chains contain both glass and rubber particles, whereas in the case of lower rubber content, ν ≲ 0.3, many chains with only stiff particles are being identified. Although the chain length remains approximately the same among the identified chains, the chains of ν ≳ 0.4 are much softer, which leads to a dramatic change in the wave speed (modulus).
Comparing the length of the chains (glass only) at lower rubber content (ν ≲ 0.3) for three different realizations confirmed that the particles’ arrangements for samples with ν ≈ 0.1 and 0.2 provide shorter (i.e., straight/stiff) chains. This can be correlated with the fact that the glass subnetworks of these two samples are in a jammed state, therefore stable. The subnetwork of the sample with ν = 0.3 is (possibly) under jamming, which makes the system less stable with weaker force chains (78). Most of the glass networks for ν ≈ 0.1 and 0.2 offer relatively short chains in comparison to ν ≈ 0.3; therefore, it is not surprising to obtain a higher modulus.
Conclusions
Recent technological developments have enabled the image-based characterization of granular materials at controlled stress states with grain-scale resolution using µXRCT. The current study aimed to understand the effect of granular mixture morphology on the macromechanical response of the assemblies by combining ultrasound propagation and image-based µXRCT characterization. In particular, the nonclassical mixture rule was discussed by combining effective properties with morphological characterization.
First, the wave propagation technique was used to analyze the mechanical response (small-strain stiffness) of mixtures of stiff–soft particulate systems. The effect of the stiff–soft composition on the compressive elastic modulus (P-wave modulus) was shown by means of wave propagation at different uniaxial preload levels. The results showed that low proportions of soft particles can enhance the modulus of the mixtures relative to the stiff-only packings. Adding more soft particles into the assemblies led to a transition from a stiff- to a soft-dominated regime where the bulk behavior of samples is mainly controlled by the soft phase. However, the macrobehavior of such granular samples can hardly be understood without microstructural information.
Next, to correlate the macrobehavior of samples with their microstructures, in situ µXRCT was conducted. Analyzing images clarified the underlying reason behind the transition mechanism from a stiff to a soft-controlled medium by separating glass and rubber subnetworks. The coordination number, i.e., the average number of contacts, provided a qualitative indication of the transition from a stiff-dominated to soft-dominated medium. The coordination number of packings, considering both glass and rubber, remained almost the same throughout different rubber fractions. The topology study of samples after image analysis showed that rubber plays a vital role in low rubber content samples, where the M-modulus stiffens 0.1 ≲ ν ≲ 0.2, by straightening/shortening the glass-only chains.
The µXRCT images provided insights into the chains’ structure. We explained the stiffness improvement adding a small amount of soft particles and the sudden drop occurring in the M-modulus at ν ≈ 0.4. Samples with ν ≲ 0.3 offer chains made of only glass particles, whereas 0.4 ≲ ν cannot offer stiff chains, i.e., made only from glass particles. The existence of rubber particles in chains of ν = 0.4, 0.5, and 0.6 softens the overall response of the samples; thus, the M-modulus has been weakened. This pioneering output has significant implications for designing materials with high stiffness and low weight, e.g., roads, where a lighter damper material with high stiffness is desired.
Understanding the microstructure of the networks of mixtures and its impact on the effective mechanical behavior of the assemblies will aid more accurate computer modeling [e.g., Discrete Element Modeling (79–81) of stiff–soft interactions] and theories (e.g., mixture theories of porous media) by providing insights into the fundamental mechanisms that govern the behavior of such materials under different conditions. This information can be used to optimize the composition and processing of the material to achieve properties. Although both ultrasound experiments and µXRCT-imaging have provided vital details on the mixtures, some aspects, like the evolution of the microstructure under different loading conditions, remain an open question. In the future, we plan to employ material point method (34, 35, 82) simulations of wave propagation through mixtures based on µXRCT data to expand our micro–macro horizons.
Materials and Methods
Ultrasound Propagation Setup.
Low-frequency ultrasound propagation using broadband piezoelectric transducers is a nondestructive way to investigate the small-strain (compression) stiffness of granular materials (14, 83). In the present contribution, cylindrical samples consisting of monodisperse soft (rubber) and stiff (glass) particles with diameters of 4 mm are poured into a custom-made X-ray transparent oedometer cell made of polymethyl methacrylate (PMMA). Glass and rubber beads used in this study are similar to those employed in an earlier study (30, 40), with Young’s moduli of 65 GPa and 0.185 GPa, and Poisson’s ratios of 0.2 and 0.5 for glass and rubber, respectively. The cell holds cylindrical samples with a length Lz0 = 80 mm and a diameter D = 80 mm with initial volume that are then placed under uniaxial static compression. A pair of P-wave broadband piezoelectric transducers with a frequency of 100 kHz (Olympus-Panametrics Videoscan V1011) are mounted on top and bottom of the cell and connected to an ultrasonic square wave pulser/receiver unit (Olympus-Panametrics 5077PR). The amplified signals were recorded with a resolution of 15 bit and a sampling rate of 125 Ms/s using a digital oscilloscope (PicoScope 5444B). To improve the signal-to-noise ratio, 32 signals were averaged. Samples composed of various rubber fractions ranging from ν = 0 to 1 in 0.1 increments were prepared, where the total volume of the cylinder is occupied by glass particles when ν= 0 and by rubber particles when ν = 1. The samples were prestressed in a gradual manner using static mechanical force. At different quasistatic axial stresses, p = 40, 80, 120, 160, 200 kPa, acoustic P-waves are propagated from the top transducer (source) into the prepared samples, and the bottom transducer (receiver) collects the signals. To ensure reproducibility, each mixture was repeated five times, with particles being removed and added to the cell each time to obtain a new particle arrangement and eliminate configuration dependency.
Micro-X-Ray Computed Tomography.
µXRCT imaging (84, 85) is arguably the most promising approach to attain the 3D microstructure of particle packings in high resolution by reconstructing the internal structure from a high number of 2D projection images (radiograms) acquired from different directions. The main advantage of µXRCT imaging in comparison to other nondestructive imaging methods (e.g., magnetic resonance imaging) is its ability to resolve the internal microstructure with high accuracy (86, 87). It is generally possible to visualize features down to the single-digit micrometer range (84, 85). Thus, it has been widely used to attain microscopic features of particulate systems. To further enhance a micromechanical insight into the mixture packings, the phase transition from stiff- to soft-dominated (0.1 ≤ ν ≤ 0.6), and the stiffening behavior of the packings with a low number of soft inclusions (0.1 ≤ ν ≤ 0.2), at stresses of 80 kPa and 160 kPa, approximately, were visualized by in situ µXRCT. For this, a lab-based modular buildup µXRCT system further described in ref. 88 was used. The underlying used experimental setup is illustrated in Fig. 6A showing the combination of conventional imaging setup and wave propagation measurements into an oedometer cell under uniaxial preload. It is worth mentioning that due to the existence of rubber particles, it is not possible to apply diffraction measurements of contact fabric, i.e., interparticle force, on the samples.
Fig. 6.

Unlike wave propagation tests, µXRCT scans are expensive both in energy consumption and time. Thus, we performed µXRCT scans on two vertical stresses p= 80 kPa and 160 kPa. Nevertheless, three different configurations (networks) were prepared for samples with rubber fractions ν = 0.1, 0.2, and 0.3, whereas for samples with rubber fractions ν = 0.4, 0.5, and 0.6, only one test was performed. All 24 (two vertical stresses × six rubber contents, 3× ν : {0.1, 0.2, 03} + 1× ν : {0.4, 0.5, 06}) scans were performed with identical image acquisition settings. To capture the whole cell content (D = 80 mm; Lz0 = 80 mm), a geometric magnification of 1.36 was used, given by the ratio of source–detector distance and source–object distance. Using 2 × 2 detector binning, the final resulting voxel edge length is 149.6 µm and sufficiently high to resolve the beads having a 4 mm diameter. The X-ray tube voltage and flux were set to 110 kV and 110 µA, and the detector exposure time to 1,000 ms. For the scan, the loaded sample was rotated 180° clockwise and counterclockwise in 0.25° increments to cover the necessary complete turn. To enhance the final image quality with regard to ring artifacts, two slightly shifted projections for each angle were acquired and combined. Further information on the experimental setup and the used parameters can be found in ref. 89. For each scan, stress relaxation in the order of 10 kPa occurred quickly after switching from force- to a displacement-controlled mode for the imaging. However, we observed a quick recovery of the load upon reloading. Each scan took about 120 min and was performed displacement-controlled to avoid potential movement errors. The 3D volume reconstruction based on the radiograms of each scan was done with the FDK algorithm (90) using the commercial software Octopus Reconstruction (v.8.9.4-64 bit) (91). Image processing of the reconstructed gray value image stacks was performed with Dragonfly software (v.2020.2) (92); see Fig. 6B. First, a mathematical smoothing function (median filter) was applied to reduce unwanted noise in the tomograms. Accurate segmentation of images was achieved due to the high difference in attenuation coefficients between glass, rubber, and air. Finally, glass and rubber particles were identified using a mathematical morphology technique, watershed transform, on defined markers of individual particles to determine grain volumes, grain centroids, and all contact locations and orientations (93–95). To identify contacts between particles, immediate neighbor voxels containing two distinct grain IDs were considered (96, 97). To select a so-called true contact, a minimum of 10 voxels between two particles was set as a threshold for a contact candidate (87, 95).
For further analysis, we demonstrate the samples only at p = 160 kPa since the topological response of p = 80 kPa is almost unchanged. Results of the analysis of p = 80 kPa are reported in supplementary information file. The in situ acquired data of all scanned samples, including metadata, are open-access published (98–101); see SI Appendix for more details.
Data, Materials, and Software Availability
The dataset includes stacks of gray value images in 16-bit *.tif format, along with the measured/applied force and displacement over time provided in *.csv files. Additionally, the dataset contains the measured signal data of the ultrasonic transducer pair over time, which is stored in *.csv files. These files contain the average of 32 acquired signals, aimed at enhancing the signal-to-noise ratio. All the aforementioned data has been deposited in the Data Repository of the University of Stuttgart (DaRUS) and can be accessed through the corresponding references (98–101).
Acknowledgments
We thank Lou Kondic for many valuable discussions on networks and topology of granular materials, and Farhang Radjai, Saeid Nezamabadi, and Kuniyasu Saitoh for our collaborations and discussions on particle simulations of granular mixtures. We acknowledge the funding by the German Research Foundation (DFG) through the project STE-969/16-1 (project No. 424876160) within the SPP 1897 “Calm, Smooth and Smart—Novel Approaches for Influencing Vibrations by Means of Deliberately Introduced Dissipation.” M.R. and H.S. acknowledge funding from the DFG through Project No. 357361983. H.S. thanks the DFG for supporting this work under Grant No. SFB 1313 (Project No. 327154368). We also express our sincere gratitude to the anonymous reviewers for their valuable comments, suggestions, and constructive criticism. Their expert insights and feedback have undoubtedly helped to improve the quality of this work and have contributed significantly to its overall impact.
Author contributions
K.T., M.R., and H.S. designed research; K.T. and M.R. performed research; K.T. contributed new reagents/analytic tools; K.T. analyzed data; S.L. contributed to discussions; H.S. coordinated the research; S.L. and H.S. revised the paper; K.T. and M.R. wrote the paper.
Competing interests
The authors declare no competing interest.
Supporting Information
Appendix 01 (PDF)
- Download
- 583.66 KB
References
1
K. E. Daniels, N. W. Hayman, Force chains in seismogenic faults visualized with photoelastic granular shear experiments. J. Geophys. Res.: Solid Earth 113, B11411 (2008).
2
L. Papadopoulos, M. A. Porter, K. E. Daniels, D. S. Bassett, Network analysis of particles and grains. J. Complex Networks 6, 485–565 (2018).
3
R. Behringer et al., Statistical properties of granular materials near jamming. J. Stat. Mech.: Theory Exp. 2014, P06004 (2014).
4
S. Luding, K. Taghizadeh, C. Cheng, L. Kondic, Understanding slow compression and decompression of frictionless soft granular matter by network analysis. Soft Matter 18, 1868–1884 (2022).
5
K. Aki, P. G. Richards, Quantitative Seismology (University Science Books, California, 2002).
6
B. O. Hardin, F. Richart Jr., Elastic wave velocities in granular soils. J. Soil Mech. Found. Div. 89, 33–65 (1963).
7
J. Hall Jr., F. Richart Jr., Dissipation of elastic wave energy in granular soils. J. Soil Mech. Found. Div. 89, 27–56 (1963).
8
J. S. Lee, J. C. Santamarina, Bender elements: Performance and signal interpretation. J. Geotech. Geoenviron. Eng. 131, 1063–1070 (2005).
9
V. Magnanimo et al., Characterizing the shear and bulk moduli of an idealized granular material. Europhys. Lett. (EPL) 81, 34006 (2008).
10
V. Magnanimo, “Wave propagation and elasticity in granular soils: A numerical approach for a micromechanical perspective” in Views on Microstructures in Granular Materials (Springer, 2020), pp. 107–135.
11
H. A. Makse, N. Gland, D. L. Johnson, L. M. Schwartz, Why effective medium theory fails in granular materials. Phys. Rev. Lett. 83, 5070 (1999).
12
C. Goldenberg, I. Goldhirsch, Force chains, microelasticity, and macroelasticity. Phys. Rev. Lett. 89, 084302 (2002).
13
J. D. Goddard, Nonlinear elasticity and pressure-dependent wave speeds in granular media. Proc. R. Soc. A 430, 105–131 (1990).
14
K. Walton, The effective elastic moduli of a random packing of spheres. J. Mech. Phys. Solids 35, 213–226 (1987).
15
A. Misra, C. S. Chang, Effective elastic moduli of heterogeneous granular solids. Int. J. Solids Struct. 30, 2547–2566 (1993).
16
J. Jenkins, D. Johnson, L. La Ragione, H. Makse, Fluctuations and the effective moduli of an isotropic, random aggregate of identical, frictionless spheres. J. Mech. Phys. Solids 53, 197–225 (2005).
17
L. La Ragione, J. T. Jenkins, The initial response of an idealized granular material. Proc. R. Soc. A 463, 735–758 (2007).
18
N. P. Kruyt, I. Agnolin, S. Luding, L. Rothenburg, Micromechanical study of elastic moduli of loose granular materials. J. Mech. Phys. Solids 58, 1286–1301 (2010).
19
X. Tang, J. Yang, Wave propagation in granular material: What is the role of particle shape? J. Mech. Phys. Solids 157, 104605 (2021).
20
D. Liu, C. O’Sullivan, J. A. H. Carraro, Use of combined static and dynamic testing to quantify the participation of particles in stress transmission. J. Geotech. Geoenviron. Eng. 148, 04022100 (2022).
21
M. Otsubo, T. T. Dutta, M. Durgalian, R. Kuwano, C. O’Sullivan, “Particle-scale insight into transitional behaviour of gap-graded materials—Small-strain stiffness and frequency response” in E3S Web of Conferences (EDP Sciences, 2019), vol. 92, p. 14006.
22
E. T. Owens, K. E. Daniels, Acoustic measurement of a granular density of modes. Soft Matter 9, 1214–1219 (2013).
23
J. R. Valdes, T. M. Evans, Sand–rubber mixtures: Experiments and numerical simulations. Can. Geotech. J. 45, 588–595 (2008).
24
K. Taghizadeh, H. Steeb, V. Magnanimo, S. Luding, “Elastic waves in particulate glass–rubber mixture: Experimental and numerical investigations/studies” in EPJ Web of Conferences (EDP Sciences, 2017), vol. 140, p. 12019.
25
Z. Cheng, J. Wang, W. Li, The micro-mechanical behaviour of sand-rubber mixtures under shear: An experimental study based on X-ray micro-tomography. Soils Found. 60, 1251–1268 (2020).
26
A. Platzer, S. Rouhanifar, P. Richard, B. Cazacliu, E. Ibraim, Sand–rubber mixtures undergoing isotropic loading: Derivation and experimental probing of a physical model. Granular Matter 20, 1–10 (2018).
27
I. Benessalah, A. Arab, M. Sadek, R. Bouferra, Laboratory study on the compressibility of sand–rubber mixtures under one dimensional consolidation loading conditions. Granular Matter 21, 1–9 (2019).
28
A. Ari, S. Akbulut, Effect of particle size and shape on shear strength of sand–rubber granule mixtures. Granular Matter 24, 1–20 (2022).
29
M. Cárdenas-Barrantes, J. Barés, M. Renouf, É. Azéma, Experimental validation of a micromechanically based compaction law for mixtures of soft and hard grains. Phys. Rev. E 106, L022901 (2022).
30
K. Giannis et al., Stress based multi-contact model for discrete-element simulations. Granular Matter 23, 1–14 (2021).
31
M. Cárdenas-Barrantes, D. Cantor, J. Barés, M. Renouf, E. Azéma, Three-dimensional compaction of soft granular packings. Soft Matter 18, 312–321 (2022).
32
J. L. Perez, C. Kwok, K. Senetakis, Effect of rubber size on the behaviour of sand–rubber mixtures: A numerical investigation. Comput. Geotech. 80, 199–214 (2016).
33
T. L. Vu, S. Nezamabadi, S. Mora, Effects of particle compressibility on structural and mechanical properties of compressed soft granular materials. J. Mech. Phys. Solids 146, 104201 (2021).
34
S. Nezamabadi, T. H. Nguyen, J. Y. Delenne, F. Radjai, Modeling soft granular materials. Granular Matter 19, 1–12 (2017).
35
S. Nezamabadi, F. Radjai, J. Averseng, J. Y. Delenne, Implicit frictional–contact model for soft particle systems. J. Mech. Phys. Solids 83, 72–87 (2015).
36
J. Zhang, X. Chen, J. Zhang, P. Jitsangiam, X. Wang, Dem investigation of macro- and micro-mechanical properties of rigid-grain and soft-chip mixtures. Particuology 55, 128–139 (2021).
37
O. Bouillanne et al., How vorticity and agglomeration control shear strength in soft cohesive granular flows. Granular Matter 24, 1–17 (2022).
38
Z. Hu, Y. Shi, N. Guo, Z. Yang, Micromechanical investigation of the shear behaviors of sand–rubber mixtures using a multibody meshfree method. Granular Matter 24, 1–15 (2022).
39
H. K. Kim, J. C. Santamarina, Sand–rubber mixtures (large rubber chips). Can. Geotech. J. 45, 1457–1466 (2008).
40
K. Taghizadeh, H. Steeb, S. Luding, V. Magnanimo, Elastic waves in particulate glass–rubber mixtures. Proc. R. Soc. A 477, 20200834 (2021).
41
R. C. Hidalgo, C. U. Grosse, F. Kun, H. W. Reinhardt, H. J. Herrmann, Evolution of percolating force chains in compressed granular media. Phys. Rev. Lett. 89, 205501 (2002).
42
K. Krishnaraj, P. R. Nott, Coherent force chains in disordered granular materials emerge from a percolation of quasilinear clusters. Phys. Rev. Lett. 124, 198002 (2020).
43
S. C. Cowin, The relationship between the elasticity tensor and the fabric tensor. Mech. Mater. 4, 137–147 (1985).
44
D. S. Bassett, E. T. Owens, K. E. Daniels, M. A. Porter, Influence of network topology on sound propagation in granular materials. Phys. Rev. E 86, 041306 (2012).
45
A. M. Booth, R. Hurley, M. P. Lamb, J. E. Andrade, Force chains as the link between particle and bulk friction angles in granular material. Geophys. Res. Lett. 41, 8862–8869 (2014).
46
L. Kondic et al., Topology of force networks in compressed granular media. Europhys. Lett. 97, 54001 (2012).
47
D. M. Walker et al., Structural templates of disordered granular media. Int. J. Solids. Struct. 54, 20–30 (2015).
48
V. Richefeu, M. S. El Youssoufi, E. Azéma, F. Radjai, Force transmission in dry and wet granular media. Powder Technol. 190, 258–263 (2009).
49
C. Voivret, F. Radjai, J. Y. Delenne, M. S. El Youssoufi, Multiscale force networks in highly polydisperse granular media. Phys. Rev. Lett. 102, 178001 (2009).
50
L. Zhang, Y. Wang, J. Zhang, Force-chain distributions in granular systems. Phys. Rev. E 89, 012203 (2014).
51
J. Peters, M. Muthuswamy, J. Wibowo, A. Tordesillas, Characterization of force chains in granular material. Phys. Rev. E 72, 041307 (2005).
52
S. Schmidt, M. Wiebicke, I. Herle, On the determination and evolution of fabric in representative elementary volumes for a sand specimen in triaxial compression. Granular Matter 24, 1–9 (2022).
53
M. Wiebicke, I. Herle, E. Andò, G. Viggiani, Measuring the fabric evolution of sand-application and challenges. Geotechnik 44, 114–122 (2021).
54
B. Zhao, J. Wang, E. Andò, G. Viggiani, M. R. Coop, Investigation of particle breakage under one-dimensional compression of sand using X-ray microtomography. Can. Geotech. J. 57, 754–762 (2020).
55
Z. Karatza, E. Andò, S. A. Papanicolopulos, G. Viggiani, J. Y. Ooi, Effect of particle morphology and contacts on particle breakage in a granular assembly studied using X-ray tomography. Granular Matter 21, 1–13 (2019).
56
D. Lee, N. Karadimitriou, M. Ruf, H. Steeb, Detecting micro fractures: A comprehensive comparison of conventional and machine-learning-based segmentation methods. Solid Earth 13, 1475–1494 (2022).
57
Y. Xing et al., X-ray tomography investigation of cyclically sheared granular materials. Phys. Rev. Lett. 126, 048002 (2021).
58
S. Hasan et al., Direct characterization of solute transport in unsaturated porous media using fast X-ray synchrotron microtomography. Proc. Natl. Acad. Sci. U.S.A. 117, 23443–23449 (2020).
59
J. Baker, F. Guillard, B. Marks, I. Einav, X-ray rheography uncovers planar granular flows despite non-planar walls. Nat. Commun. 9, 1–9 (2018).
60
S. A. Hall et al., Can intergranular force transmission be identified in sand? Granular Matter 13, 251–254 (2011).
61
R. Hurley, S. Hall, J. Andrade, J. Wright, Quantifying interparticle forces and heterogeneity in 3D granular materials. Phys. Rev. Lett. 117, 098005 (2016).
62
C. Zhai et al., Quantifying local rearrangements in three-dimensional granular materials: Rearrangement measures, correlations, and relationship to stresses. Phys. Rev. E 105, 014904 (2022).
63
P. Wochner et al., X-ray cross correlation analysis uncovers hidden local symmetries in disordered matter. Proc. Natl. Acad. Sci. U.S.A. 106, 11511–11514 (2009).
64
M. Asadi, A. Mahboubi, K. Thoeni, Discrete modeling of sand–tire mixture considering grain-scale deformability. Granular Matter 20, 1–13 (2018).
65
M. Asadi, K. Thoeni, A. Mahboubi, An experimental and numerical study on the compressive behavior of sand–rubber particle mixtures. Comput. Geotech. 104, 185–195 (2018).
66
A. Ikeda, T. Kawasaki, L. Berthier, K. Saitoh, T. Hatano, Universal relaxation dynamics of sphere packings below jamming. Phys. Rev. Lett. 124, 058001 (2020).
67
P. Rissone, E. I. Corwin, G. Parisi, Long-range anomalous decay of the correlation in jammed packings. Phys. Rev. Lett. 127, 038001 (2021).
68
N. Kumar, S. Luding, Memory of jamming-multiscale models for soft and granular matter. Granular Matter 18, 1–21 (2016).
69
D. Bi, J. Zhang, B. Chakraborty, R. P. Behringer, Jamming by shear. Nature 480, 355–358 (2011).
70
S. Luding, So much for the jamming point. Nat. Phys. 12, 531–532 (2016).
71
R. P. Behringer, B. Chakraborty, The physics of jamming for granular materials: A review. Rep. Prog. Phys. 82, 012601 (2018).
72
F. Göncü, S. Luding, Effect of particle friction and polydispersity on the macroscopic stress–strain relations of granular materials. Acta Geotech. 8, 629–643 (2013).
73
K. Taghizadeh Bajgirani, “Elasticity and wave propagation in granular materials,” PhD thesis, University of Twente (2019).
74
E. T. Owens, K. E. Daniels, Sound propagation and force chains in granular materials. Europhys. Lett. 94, 54005 (2011).
75
C. Zhai, E. B. Herbold, R. C. Hurley, The influence of packing structure and interparticle forces on ultrasound transmission in granular media. Proc. Natl. Acad. Sci. U.S.A. 117, 16234–16242 (2020).
76
A. H. Clark, A. J. Petersen, L. Kondic, R. P. Behringer, Nonlinear force propagation during granular impact. Phys. Rev. Lett. 114, 144502 (2015).
77
J. Liu, A. Wautier, S. Bonelli, F. Nicot, F. Darve, Macroscopic softening in granular materials from a mesoscale perspective. Int. J. Solids Struct. 193, 222–238 (2020).
78
D. M. Walker et al., Percolating contact subnetworks on the edge of isostaticity. Granular Matter 13, 233–240 (2011).
79
S. Luding, Introduction to discrete element methods: Basic of contact force models and how to perform the micro–macro transition to continuum theory. Eur. J. Environ. Civil Eng. 12, 785–826 (2008).
80
K. Taghizadeh, S. Luding, V. Magnanimo, DEM applied to soil mechanics. ALERT Doctoral School 2017 Discrete Element Modeling (2017), p. 129.
81
F. Radjai, F. Dubois, Discrete-Element Modeling of Granular Materials (Wiley-ISTE, 2011).
82
A. Larese, I. Iaconeta, B. Chandra, V. Singer, Implicit MPM and coupled MPM–FEM in geomechanics. Comput. Mech. 175, 226–232 (2019).
83
X. Jia, Codalike multiple scattering of elastic waves in dense granular media. Phys. Rev. Lett. 93, 154303 (2004).
84
S. R. Stock, Micro-Computed Tomography: Methodology and Applications (CRC Press, Boca Raton, FL, ed. 2, 2019).
85
P. J. Withers et al., X-ray computed tomography. Nat. Rev. Methods Primers 1, 18 (2021).
86
I. Zanette et al., X-ray microtomography using correlation of near-field speckles for material characterization. Proc. Natl. Acad. Sci. U.S.A. 112, 12569–12573 (2015).
87
E. Andò, S. A. Hall, G. Viggiani, J. Desrues, P. Bésuelle, Grain-scale experimental investigation of localised deformation in sand: A discrete particle tracking approach. Acta Geotech. 7, 1–13 (2012).
88
M. Ruf, H. Steeb, An open, modular, and flexible micro X-ray computed tomography system for research. Rev. Sci. Instrum. 91, 113102 (2020).
89
M. Ruf, K. Taghizadeh, H. Steeb, Multi-scale characterization of granular media by in situ laboratory X-ray computed tomography. GAMM-Mitteilungen 45, e202200011
90
L. A. Feldkamp, L. C. Davis, J. W. Kress, Practical cone-beam algorithm. J. Opt. Soc. Am. A 1, 612 (1984).
91
J. Vlassenbroeck et al., Software tools for quantification of X-ray microtomography at the UGCT. Nucl. Instrum. Methods Phys. Res. Sec. A 580, 442–445 (2007).
92
Dragonfly 2021.1. Object Research Systems (ORS) Inc., Montreal, QC, Canada, Dragonfly 3.1 (computer software) (2022).
93
A. G. Athanassiadis et al., X-ray tomography system to investigate granular materials during mechanical loading. Rev. Sci. Instrum. 85, 083708 (2014).
94
I. Vlahinić, E. Andò, G. Viggiani, J. E. Andrade, Towards a more accurate characterization of granular media: Extracting quantitative descriptors from tomographic images. Granular Matter 16, 9–21 (2014).
95
M. Wiebicke, E. Andò, I. Herle, G. Viggiani, On the metrology of interparticle contacts in sand from X-ray tomography images. Meas. Sci. Technol. 28, 124007 (2017).
96
M. Wiebicke, E. Andò, V. Šmilauer, I. Herle, G. Viggiani, A benchmark strategy for the experimental measurement of contact fabric. Granular Matter 21, 1–13 (2019).
97
M. Wiebicke, E. Andò, G. Viggiani, I. Herle, Measuring the evolution of contact fabric in shear bands with X-ray tomography. Acta Geotech. 15, 79–93 (2020).
98
M. Ruf, K. Taghizadeh, H. Steeb, micro-XRCT data sets and in situ measured ultrasonic wave propagation of a pre-stressed monodisperse rubber and glass particle mixture with 50% volume rubber content (2021). https://doi.org/10.18419/DARUS-2208. Accessed 26 September 2022.
99
M. Ruf, K. Taghizadeh, H. Steeb, micro-XRCT data sets and in situ measured ultrasonic wave propagation of a pre-stressed monodisperse rubber and glass particle mixture with 30% volume rubber content (2022). https://doi.org/10.18419/DARUS-2833. Accessed 30 November 2021.
100
M. Ruf, K. Taghizadeh, H. Steeb, micro-XRCT data sets and in situ measured ultrasonic wave propagation of pre-stressed monodisperse rubber and glass particle mixtures with 10%, 20%, 40%, and 60% volume rubber content: Sample 1 (2023). https://doi.org/10.18419/DARUS-3436. Accessed 4 May 2023.
101
M. Ruf, K. Taghizadeh, H. Steeb, micro-XRCT data sets and in situ measured ultrasonic wave propagation of pre-stressed monodisperse rubber and glass particle mixtures with 10%, 20%, and 30% volume rubber content: Samples 2 and 3 (2023). https://doi.org/10.18419/DARUS-3437. Accessed 4 May 2023.
Information & Authors
Information
Published in
Classifications
Copyright
Copyright © 2023 the Author(s). Published by PNAS. This article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).
Data, Materials, and Software Availability
The dataset includes stacks of gray value images in 16-bit *.tif format, along with the measured/applied force and displacement over time provided in *.csv files. Additionally, the dataset contains the measured signal data of the ultrasonic transducer pair over time, which is stored in *.csv files. These files contain the average of 32 acquired signals, aimed at enhancing the signal-to-noise ratio. All the aforementioned data has been deposited in the Data Repository of the University of Stuttgart (DaRUS) and can be accessed through the corresponding references (98–101).
Submission history
Received: November 23, 2022
Accepted: May 21, 2023
Published online: June 20, 2023
Published in issue: June 27, 2023
Keywords
Acknowledgments
We thank Lou Kondic for many valuable discussions on networks and topology of granular materials, and Farhang Radjai, Saeid Nezamabadi, and Kuniyasu Saitoh for our collaborations and discussions on particle simulations of granular mixtures. We acknowledge the funding by the German Research Foundation (DFG) through the project STE-969/16-1 (project No. 424876160) within the SPP 1897 “Calm, Smooth and Smart—Novel Approaches for Influencing Vibrations by Means of Deliberately Introduced Dissipation.” M.R. and H.S. acknowledge funding from the DFG through Project No. 357361983. H.S. thanks the DFG for supporting this work under Grant No. SFB 1313 (Project No. 327154368). We also express our sincere gratitude to the anonymous reviewers for their valuable comments, suggestions, and constructive criticism. Their expert insights and feedback have undoubtedly helped to improve the quality of this work and have contributed significantly to its overall impact.
Author contributions
K.T., M.R., and H.S. designed research; K.T. and M.R. performed research; K.T. contributed new reagents/analytic tools; K.T. analyzed data; S.L. contributed to discussions; H.S. coordinated the research; S.L. and H.S. revised the paper; K.T. and M.R. wrote the paper.
Competing interests
The authors declare no competing interest.
Notes
This article is a PNAS Direct Submission.
Authors
Metrics & Citations
Metrics
Altmetrics
Citations
Cite this article
X-ray 3D imaging–based microunderstanding of granular mixtures: Stiffness enhancement by adding small fractions of soft particles, Proc. Natl. Acad. Sci. U.S.A.
120 (26) e2219999120,
https://doi.org/10.1073/pnas.2219999120
(2023).
Copied!
Copying failed.
Export the article citation data by selecting a format from the list below and clicking Export.
Cited by
Loading...
View Options
View options
PDF format
Download this article as a PDF file
DOWNLOAD PDFLogin options
Check if you have access through your login credentials or your institution to get full access on this article.
Personal login Institutional LoginRecommend to a librarian
Recommend PNAS to a LibrarianPurchase options
Purchase this article to access the full text.