| Literature DB >> 15600883 |
Detlef Lohse1, Raymond Bergmann, René Mikkelsen, Christiaan Zeilstra, Devaraj van der Meer, Michel Versluis, Ko van der Weele, Martin van der Hoef, Hans Kuipers.
Abstract
Very fine sand is prepared in a well-defined and fully decompactified state by letting gas bubble through it. After turning off the gas stream, a steel ball is dropped on the sand. On impact of the ball, sand is blown away in all directions ("splash") and an impact crater forms. When this cavity collapses, a granular jet emerges and is driven straight into the air. A second jet goes downwards into the air bubble entrained during the process, thus pushing surface material deep into the ground. The air bubble rises slowly towards the surface, causing a granular eruption. In addition to the experiments and the discrete particle simulations we present a simple continuum theory to account for the void collapse leading to the formation of the upward and downward jets.Year: 2004 PMID: 15600883 DOI: 10.1103/PhysRevLett.93.198003
Source DB: PubMed Journal: Phys Rev Lett ISSN: 0031-9007 Impact factor: 9.161