Pneumatic fractures in confined granular media

Fredrik K. Eriksen, Renaud Toussaint, Antoine L. Turquet, Knut J. Måløy, and Eirik G. Flekkøy
Phys. Rev. E 95, 062901 – Published 12 June 2017
PDFHTMLExport Citation

Abstract

We perform experiments where air is injected at a constant overpressure Pin, ranging from 5 to 250 kPa, into a dry granular medium confined within a horizontal linear Hele-Shaw cell. The setup allows us to explore compacted configurations by preventing decompaction at the outer boundary, i.e., the cell outlet has a semipermeable filter such that beads are stopped while air can pass. We study the emerging patterns and dynamic growth of channels in the granular media due to fluid flow, by analyzing images captured with a high speed camera (1000 images/s). We identify four qualitatively different flow regimes, depending on the imposed overpressure, ranging from no channel formation for Pin below 10 kPa, to large thick channels formed by erosion and fingers merging for high Pin around 200 kPa. The flow regimes where channels form are characterized by typical finger thickness, final depth into the medium, and growth dynamics. The shape of the finger tips during growth is studied by looking at the finger width w as function of distance d from the tip. The tip profile is found to follow w(d)dβ, where β=0.68 is a typical value for all experiments, also over time. This indicates a singularity in the curvature d2d/dw2κd12β, but not of the slope dw/dddβ1, i.e., more rounded tips rather than pointy cusps, as they would be for the case β>1. For increasing Pin, the channels generally grow faster and deeper into the medium. We show that the channel length along the flow direction has a linear growth with time initially, followed by a power-law decay of growth velocity with time as the channel approaches its final length. A closer look reveals that the initial growth velocity v0 is found to scale with injection pressure as v0Pin32, while at a critical time tc there is a cross-over to the behavior v(t)tα, where α is close to 2.5 for all experiments. Finally, we explore the fractal dimension of the fully developed patterns. For example, for patterns resulting from intermediate Pin around 100–150 kPa, we find that the box-counting dimensions lie within the range DB[1.53,1.62], similar to viscous fingering fractals in porous media.

  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
8 More
  • Received 19 October 2016
  • Revised 22 May 2017

DOI:https://doi.org/10.1103/PhysRevE.95.062901

©2017 American Physical Society

Physics Subject Headings (PhySH)

Fluid DynamicsCondensed Matter, Materials & Applied PhysicsPolymers & Soft Matter

Authors & Affiliations

Fredrik K. Eriksen*, Renaud Toussaint, and Antoine L. Turquet

  • Institut de Physique du Globe de Strasbourg, Université de Strasbourg/EOST, Centre National de la Recherche Scientifique, 67084 Strasbourg, France

Knut J. Måløy and Eirik G. Flekkøy

  • PoreLab, Department of Physics, University of Oslo, P.O. Box 1074 Blindern, 0316 Oslo, Norway

  • *Also at PoreLab, Department of Physics, University of Oslo, 0316 Oslo, Norway; f.k.eriksen@fys.uio.no

Article Text (Subscription Required)

Click to Expand

Supplemental Material (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 95, Iss. 6 — June 2017

Reuse & Permissions
Access Options
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review E

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×