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Soft granular particles sheared at a controlled volume: rate-dependent dynamics and the solid-fluid transition
J-C Tsai1, M-R Chou2, P-C Huang2
1Institute of Physics, Academia Sinica, Taipei, Taiwan. jctsai@phys.sinica.edu.tw ajrhuang@gate.sinica.edu.tw.
This study reveals distinct flow behaviors in soft hydrogel suspensions under shear, differentiating between yielding networks and fluid-mediated sliding. These findings impact our understanding of dense soft matter dynamics.
Area of Science:
- Soft Matter Physics
- Rheology
- Granular Materials
Background:
- Understanding the flow of soft particle suspensions is crucial for materials science and engineering.
- Granular suspensions exhibit complex behaviors near the jamming transition, influenced by particle softness and interstitial fluid.
Purpose of the Study:
- To investigate the rheological response of fluid-immersed soft hydrogel spheres under shear.
- To characterize the transition from solid-like to fluid-like behavior in these suspensions.
- To explore the influence of particle softness and interstitial fluid on flow dynamics.
Main Methods:
- Controlled shearing of hydrogel spheres between rough cones.
- Sudden shear cessations coupled with internal imaging.
- Flow-curve measurements and stress residue analysis.
- Determination of yield stress and solid-fluid transition points.
Main Results:
- Distinct flow regimes identified: quasi-static yielding of networks vs. fluid-mediated particle sliding.
- A continuous transition in particle settling observed with changing shear rate at high volume fractions.
- Solid-fluid transition confirmed via stress extrapolation and particle settling dynamics.
- Verification of a power law relating characteristic stress to proximity from jamming.
Conclusions:
- Soft particle dynamics involve multiple relaxation timescales, challenging existing paradigms for dense systems.
- The interplay between particle softness, interstitial fluid, and shear rate dictates suspension behavior.
- Further research is needed to extend current models to account for active softness in dense flows.
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