Accretion Dynamics on Wet Granular Materials
arXiv:1705.07783 · doi:10.1103/PhysRevLett.118.208001
Abstract
Wet granular aggregates are common precursors of construction materials, food, and health care products. The physical mechanisms involved in the mixing of dry grains with a wet substrate are not well understood and difficult to control. Here, we study experimentally the accretion of dry grains on a wet granular substrate by measuring the growth dynamics of the wet aggregate. We show that this aggregate is fully saturated and its cohesion is ensured by the capillary depression at the air-liquid interface. The growth dynamics is controlled by the liquid fraction at the surface of the aggregate and exhibits two regimes. In the viscous regime, the growth dynamics is limited by the capillary-driven flow of liquid through the granular packing to the surface of the aggregate. In the capture regime, the capture probability depends on the availability of the liquid at the saturated interface, which is controlled by the hydrostatic depression in the material. We propose a model that rationalizes our observations and captures both dynamics based on the evolution of the capture probability with the hydrostatic depression.
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Cited by in corpus (7)
- Rheology and microstructure of unsaturated granular materials: Experiments and simulations
- The simultaneous discharge of liquid and grains from a silo
- The effects of interparticle cohesion on the collapse of granular columns
- A microscopic picture of erosion and sedimentation processes in dense granular flows
- Progressive friction mobilization and enhanced Janssen's screening in confined granular rafts
- Structural similarity between dry and wet sphere packings
- Effect of an interstitial fluid on the dynamics of three-dimensional granular media