Hostname: page-component-cd9895bd7-lnqnp Total loading time: 0 Render date: 2024-12-28T05:29:28.816Z Has data issue: false hasContentIssue false

Shocks in sand flowing in a silo

Published online by Cambridge University Press:  15 February 2002

AZADEH SAMADANI
Affiliation:
Department of Physics, Clark University, Worcester, MA 01610, USA
L. MAHADEVAN
Affiliation:
Department of Applied Mathematics and Theoretical Physics, Cambridge University, Cambridge CB3 9EW, UK
A. KUDROLLI
Affiliation:
Department of Physics, Clark University, Worcester, MA 01610, USA

Abstract

We study the formation of shocks on the surface of a granular material draining through an orifice at the bottom of a quasi-two-dimensional silo. At high flow rates, the surface is observed to deviate strongly from a smooth linear inclined profile, giving way to a sharp discontinuity in the height of the surface near the bottom of the incline, the typical response of a choking flow such as encountered in a hydraulic jump in a Newtonian fluid like water. We present experimental results that characterize the conditions for the existence of such a jump, describe its structure and give an explanation for its occurrence.

Type
Research Article
Copyright
© 2002 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)