The Champati Slide

Shiva P. Pudasaini

doi:10.1063/5.0230878

2024-11-19

PRE

DOI：10.1063/5.0230878

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摘要

En 中文

Here, we report some novel findings of chute experiments with native Nepalese granular seeds, called Champatis, and when mixed with other food grain of a fundamentally different physical properties, Silam. The epitomic supergrain Champati exhibits complex frictional, spin, and rolling motion. We hypothesize that the Champati slide results in an essentially unique dynamical spreading, separation from other grains, mobility, run-out, and deposition morphology. Particularly, the surface anatomy of Champati acted vitally in characterizing these aspects. We reveal spectacular dynamical flow-obstacle interaction and depositional behavior of Champati and the mixture slide. Champati slide manifests hyper-spreading in the run-out. Soon after the mass hits the ground, the behavior is unprecedented and appears to be hardly predictable, mainly around the frontal periphery. The very special properties of Champatis control the frontal spreading, rapid grain marching, and their zig-zag sporadic motion. Particle rolling, spinning, exceptionally lower frictional energy dissipation, and grain collision played the major role resulting in an unexpectedly longer travel time and distance, explaining the astonishing hypermobility of Champati grains. The obstacle substantially changes the flow dynamics as the Champati exhibits high object mobilization capacity. Due to the unique property of the Champati, the eye-catching, amazingly strong separation of Champati from Silam evolves swiftly right after the flow inception, and the process intensifies quickly. The separation length characterizes the complex interfacial momentum exchange between the phases in the mixture. The separation length between the frontal Champatis and Silam grains increases exceptionally as it does between the main body and the exclusively Silam-covered tremendously long tail of the flow in the inclined portion of the channel. These results may be useful in better understanding the phase separation, superwide-spreading and hypermobility of some geological flows, including fragmented rock avalanches, probably helping resolve some relevant standing challenges.

Keyword:

DEBRIS FLOW

AVALANCHE

FRAGMENTATION

GERMINATION

RUNOUT