Abstract

This paper performs a numerical investigation on the kinetic behaviors of dry granular flows generated by the collapse of granular columns with different fractal particle size distributions (FPSDs) using the discrete element method. The FPSD has a remarkable impact on the regime and mobility of a granular flow. As the fractal dimension of a granular assembly increases, the translational velocities of the particles increase in the horizontal direction, whereas the rotational velocities decrease. The number of particles involved in the horizontal spreading increases due to the decreasing intensity of the contact shearing particle behavior. These increased translational velocities in the horizontal direction effectively facilitate particle spreading. A boundary layer is formed at the front bottom of the granular body in which the clockwise rotational velocities of particles are significantly increased, thereby benefiting particle spreading. The whole front of the granular flow obtains an immense spreading velocity. Moreover, the translational and rotational characteristics are dependent on the particle size. Smaller particles tend to translate and rotate faster than larger particles because of the greater particle contact forces of the former. As the fractal dimension increases, medium- and large-size particles obtain less kinetic energy than do small-size particles. Therefore, small-size particles play a crucial role in the mobility of granular flows in a granular assembly with a high fractal dimension.

Highlights

  • Dry granular flows can move far away from their initial positions

  • This paper performs a numerical investigation on the kinetic behaviors of dry granular flows generated by the collapse of granular columns with different fractal particle size distributions (FPSDs) using the discrete element method

  • The FPSD has a remarkable impact on the regime and mobility of a granular flow

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Summary

Introduction

Dry granular flows (e.g., debris and rock avalanches) can move far away from their initial positions. Over the last 40 years, many theories and mechanisms, including various lubricant effects caused by interstitial gas (Roche et al, 2011), acoustic energy (Melosh, 1979), dust dispersion (Hsü, 1975), soil and water mixtures (Hungr and Evans, 2004), frictional heating and hydraulic diffusivity (Goren and Aharonov, 2007), segregation induced by grain size (Bartali et al, 2015; Zhou et al, 2019a), and rock breakage (Langlois et al, 2015), have been proposed to describe the kinetic behaviors of granular flows The connections between these mechanisms and the particle-scale information from numerical investigations will provide profound insights. The aspect ratio was found to govern the energy evolution (Utili et al, 2015; Huang et al, 2020)

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