PulseExploreJournal ClubDebatesTrendingResearchersJournals
Instagram
HomeExploreJournal ClubTrending
Synapse
⌘+K
Synapse
January 2, 1989Physical Review Letters343 citations

Instability in a Sand Heap

View Full Paper
PÉP. ÉvesqueJRJean Rajchenbach

Key Points

  • This investigation aims to understand the conditions under which a sand heap becomes unstable when subjected to vertical vibrations.
  • Utilized low-frequency vertical vibrations with a range of 10-1000 Hz.
  • Analyzed the free surface inclination angle and particle flow in the heap.
  • Identified vibration acceleration as a key control parameter.
  • The free surface of the sand heap becomes inclined at a specific angle due to vibrations.
  • A continuous flow of particles occurs down the inclined surface.
  • Convective transport refills the top of the heap with new beads.

Abstract

When a bead heap is submitted to low-frequency (2=10-1000 Hz) vertical vibrations at a large enough amplitude a, its horizontal free surface becomes unstable and a stationary state is reached. This one is characterized firstly by a free surface which is inclined within an angle to the horizontal, secondly by a continuous flow of particles rolling down the free surface, and thirdly by a convective transport inside the material which refills the top of the heap with new beads. We demonstrate that a control parameter is the vibration acceleration =a^2.

Ask AI
Helpful
Bookmark
Share
View Full Paper

Cite This Study

Évesque et al. (1989) studied this question.

synapsesocial.com/papers/6a15452479ff98d0de4e5b0chttps://doi.org/10.1103/physrevlett.62.44
Ask AI
Helpful
Bookmark
Share
View Full Paper