Physics

Viewpoint: Jamming Grains Come Full Circle

October 7, 2019• Physics 12, 109

The characterization of a brand new transition in sheared grains helps to fill within the section diagram for granular supplies.

Figure captionexpand figure

Yiqiu Zhao/Duke College

Determine 1: A 2D granular system is positioned underneath shear stress inside a ring-shaped cell. The shear is generated by rotation of the outer wall, in addition to independently transferring concentric rings under the grains. The rotation price (crimson arrows) will increase with radius, leading to a uniform shear. On the left, the grains are imaged in white gentle, whereas on the suitable, a polarized inexperienced gentle supply is used to focus on grains which can be experiencing robust contact forces.A 2D granular system is positioned underneath shear stress inside a ring-shaped cell. The shear is generated by rotation of the outer wall, in addition to independently transferring concentric rings under the grains. The rotation price (crimson arrows) will increase with radius… Present extra

Figure caption

Yiqiu Zhao/Duke College

Determine 1: A 2D granular system is positioned underneath shear stress inside a ring-shaped cell. The shear is generated by rotation of the outer wall, in addition to independently transferring concentric rings under the grains. The rotation price (crimson arrows) will increase with radius, leading to a uniform shear. On the left, the grains are imaged in white gentle, whereas on the suitable, a polarized inexperienced gentle supply is used to focus on grains which can be experiencing robust contact forces.×

The research of granular supplies is essential for a variety of fields from business to geophysics [1]. One of many distinctive features of grains is that they’ll behave like fluids or like solids—generally switching unpredictably between the 2 phases. For instance, the grains saved in silos are presupposed to movement out of and down chutes like a fluid, however too typically solid-like arches clog the movement. Alternatively, dense packings of snow or soil can instantly rework right into a flowing avalanche or landslide. To probe these fluid-solid transitions Yiqiu Zhao from Duke College, North Carolina, and colleagues have designed a brand new “ring-shear” experiment that makes use of concentric rings to shear a 2D granular system of centimeter-wide disks [2]. The group used their information to assemble a section diagram, which reveals, for the primary time, the transition between fragile solids with fluid-like options and shear-jammed solids which can be steady in opposition to shear reversals. This fuller image of granular transitions might be helpful in creating higher, extra predictive fashions for understanding and avoiding grain-related issues and disasters.

Granular supplies are not like easy fluids or solids in that they aren’t totally described by primary macroscopic variables reminiscent of density, stress, and temperature. This distinction arises as a result of granular supplies have a microstructure—or “cloth”—that may change every time they’re disturbed [3, 4]. This microstructure evolution is obvious within the historical past dependence of the isotropic jamming density 𝜑J0. Under 𝜑J0, a granular system behaves like a fluid, however when compressed to densities above 𝜑J0, the grains kind robust power chains—linear paths of enormous contact forces—that give the fabric a solid-like inside construction. The way in which the system has been beforehand compressed determines the current chain configuration, and any new deformation can result in a plastic, irreversible change of the material—largely growing 𝜑J0 [3, 4]. Because of this, the worth of the jamming density just isn’t fastened however varies in line with the microstructure historical past [5].

To discover additional the position of the microstructure’s evolution on the macroscopic granular habits, researchers carry out experiments through which a granular materials is sheared. The standard setup is two-dimensional, with the grains confined in a flat, annular (ring) shear cell, whose outer or internal cylindrical wall rotates [6, 7]. This rotation generates shear stresses that trigger anisotropic, direction-dependent deformations and rearrangements of the microstructure. Sadly, the granular system usually splits up (bifurcates) right into a solid-like area and a extra fluid-like area, known as a shear band. This dual-phase configuration prevents researchers from exploring the poorly understood intermediate states, which presumably will provide some perception into the microstructure rearrangements that drive fluid-solid transitions, in addition to the steady-state flows [8].

Zhao and colleagues have been in a position to probe these intermediate states utilizing a brand new experimental ring-shear-cell design [2]. Their machine consists of concentric rings that rotate independently from the cell’s outer wall and from one another, producing an virtually homogeneous shear profile—no less than for grain densities that aren’t too giant. This extra uniform shear helps to observe the power chains and different microstructure options of their system. As in earlier work [6, 7, 9, 10], Zhao et al. used grains (disks) product of a photoelastic materials whose stress-dependent gentle response can be utilized to tell apart which grains are experiencing giant versus small contact forces (Fig. 1).

Of their experiments, the group elevated the shear amplitude (pressure) and noticed the onset of shear jamming [4, 9]. The shear jamming transition level 𝜑Jshearoccurred at densities under the isotropic jamming density 𝜑J0. The explanation for this decrease density threshold is that sheared grains have a looser and extra anisotropic configuration in comparison with compressed-only grains. The less-efficient packing ends in a quantity enlargement (dilatancy) that’s noticeable on the seaside when the sand being sheared underneath our ft expands and turns into dry. Nevertheless, within the confined area of the shear cell, the less-efficient packing results in a rise of stress (pressure-dilatancy), which may trigger shear jamming when the density is above 𝜑Jshear.

The group additionally checked out what occurred when the shear was reversed. At shear reversal, the system is allowed to return to configurations that it had explored earlier than. Modifications in microstructure now should result in a much less anisotropic, extra effectively packed state. If this impact is giant sufficient, unjamming occurs after reversal, and the state is termed “fragile” (which differs from the standard use of this time period [9]). Nevertheless, in different circumstances, the system stays jammed, and the state is labeled “shear jammed.” Zhao et al. discovered that—above a given shear pressure and stress—sure minimal densities, 𝜑F and 𝜑SJ, are required for the system to assist fragile states or shear-jammed states, respectively. In contrast to 𝜑J0, these transition densities should not historical past dependent, thus making it doable to pinpoint, for the primary time experimentally, the place fragile states and shear-jammed states exist within the granular materials’s section diagram and to look at the transitions between them.

The intermediate density 𝜑SJ is essentially the most putting of the system’s transition factors. When this density threshold is crossed, each the macroscopic state variables and the microscopic system descriptors (just like the variety of contacts per grain and the material anisotropy) are various qualitatively. In my view, 𝜑SJ is particular as a result of it’s the place the solid-like options win in opposition to the fluid-like options [5]. Each under and above 𝜑SJ, one has a stable contact community (sustained by the frictional base), however the stability of this community modifications from fluidly fragile to solidly shear jammed when one crosses the transition. Such an intermediate state has not been studied in any experiment to my information. The brand new outcomes permit us to determine an intermediate transition that’s usually evaded by the system that bifurcates in a unfastened shear band and a dense stable. Additional investigation of this area ought to provide insights into fluid-solid transitions, reminiscent of silo clogging and avalanches, the place compression and shear results are energetic on the similar time.

This analysis is revealed in Bodily Evaluate Letters.

References

I. Einav and A. M. Puzrin, “Strain-dependent elasticity and vitality conservation in elastoplastic fashions for soils,” J. Geotech. Geoenviron. Eng. 130, 81 (2004); Q. Zhang and Ok. Kamrin, “Microscopic description of the granular fluidity area in nonlocal movement modeling,” Phys. Rev. Lett. 118, 058001 (2017).Y. Zhao, J. Barés, H. Zheng, J. E. S. Socolar, and R. P. Behringer, “Shear-jammed, fragile, and regular states in homogeneously strained granular supplies,” Phys. Rev. Lett. 123, 158001 (2019).E. Andò, J. Dijkstra, E. Roubin, C. Dano, and E. Boller, “A peek into the origin of creep in sand,” Granul. Matter 21, 11 (2019); M. Wiebicke, E. Andò, V. Šmilauer, I. Herle, and G. Viggiani, “A benchmark technique for the experimental measurement of contact cloth,” 21, 54 (2019).N. Kumar and S. Luding, “Reminiscence of jamming–multiscale fashions for comfortable and granular matter,” Granul. Matter 18, 1 (2016).S. Luding, “A lot for the jamming level,” Nat. Phys. 12, 531 (2016).D. Howell, R. P. Behringer, and C. Veje, “Stress fluctuations in a 2D granular couette experiment: A steady transition,” Phys. Rev. Lett. 82, 5241 (1999).M. Lätzel, S. Luding, H. J. Herrmann, D. W. Howell, and R. P. Behringer, “Evaluating simulation and experiment of a 2D granular Couette shear machine,” Eur. Phys. J. E 11, 325 (2003).A. Nicolas, E. E. Ferrero, Ok. Martens, and Jean-Louis Barrat, “Deformation and movement of amorphous solids: Insights from elastoplastic fashions,” Opinions of Trendy Physics 90, 045006 (2018); M. M. Bandi, P. Das, O. Gendelman, H. G. E. Hentschel, and I. Procaccia, “Common scaling legal guidelines for shear induced dilation in frictional granular media,” Granul. Matter 21, 40 (2019); Sudeshna Roy, Stefan Luding, and T. Weinhart, “A normal(ized) native rheology for moist granular supplies,” New J. Phys. 19, 043014 (2017).D. Bi, J. Zhang, B. Chakraborty, and R. P. Behringer, “Jamming by shear,” Nature 480, 355 (2011).D. M. Walker, A. Tordesillas, J. Ren, J. A. Dijksman, and R. P. Behringer, “Uncovering temporal transitions and self-organization throughout sluggish growing older of dense granular media within the absence of shear bands,” Europhys. Lett. 107, 18005 (2014).

Concerning the Creator

Image of Stefan Luding

Stefan Luding acquired his Ph.D. from the College of Freiburg, Germany. After a postdoc at Paris IV, Jussieu, he joined the Computational Physics group on the College of Stuttgart, Germany, the place he achieved his habilitation in 1998. In 2001, he moved to DelftChemTech at Delft College of Expertise, Netherlands, as Affiliate Professor in Particle Expertise. Since 2007 he has chaired the group Multiscale Mechanics (MSM) on the School of Engineering Expertise and MESA+ on the College of Twente, Netherlands. His main analysis pursuits are granular matter, non-Newtonian movement rheology, nonlinear solids, particle interactions, cohesive powders, asphalt, composites, bio-/micro-fluid techniques, self-healing supplies, and micro-macro transition strategies.

Topic Areas

Associated Articles

Synopsis: Softening Tones Make Shear-Thickening Fluids RelaxFocus: Friction, Not Inertia, Controls AvalanchesSynopsis: Chemical Conversations Lead to Particle Cliques Extra Articles


Supply hyperlink

Show More

Related Articles

Leave a Reply

Your email address will not be published. Required fields are marked *

Close