3 Iconography
Access to the text (HTML) Access to the text (HTML)
PDF Access to the PDF text

Access to the full text of this article requires a subscription.
  • If you are a subscriber, please sign in 'My Account' at the top right of the screen.

  • If you want to subscribe to this journal, see our rates

  • You can purchase this item in Pay Per ViewPay per View - FAQ : 33,00 € Taxes included to order
    Pages Iconography Videos Other
    8 3 0 0

Comptes Rendus Physique
Volume 16, n° 1
pages 37-44 (janvier 2015)
Doi : 10.1016/j.crhy.2014.11.004
Slow granular flows: The dominant role of tiny fluctuations
Écoulements granulaires lents : Le rôle dominant des très petites fluctuations

Martin van Hecke
 Huygens-Kamerlingh Onnes Lab, Universiteit Leiden, Postbus 9504, 2300 RA Leiden, The Netherlands 


What mechanism governs slow flows of granular media? Microscopically, the grains experience enduring frictional contacts in these flows. However, a straightforward translation to a macroscopic frictional rheology, where the shear stresses are proportional to the normal stresses with a rate-independent friction coefficient, fails to capture important aspects of slow granular flows. There is now overwhelming evidence that agitations, tiny fluctuations of the grain positions, associated with large fluctuation of their contact forces, play a central role for slow granular flows. These agitations are generated in flowing regions, but travel deep inside the quiescent zones, and lead to a nonlocal rheology.

The full text of this article is available in PDF format.

Quel est le mécanisme qui gouverne les écoulements lents d'un milieu granulaire ? À l'échelle microscopique, les grains sont soumis à des contacts frottants. Cependant, une interprétation directe de ces écoulements par une rhéologie macroscopique, dans laquelle les contraintes de cisaillement seraient proportionnelles aux contraintes normales avec un coefficient de frottement indépendant de la vitesse, ne permet pas de reproduire certaines propriétés importantes des écoulements lents. Il est maintenant clair que, lorsqu'elles sont associées à de grandes fluctuations des forces de contact, de très petites fluctuations des positions des grains jouent un rôle capital dans ces écoulements. Bien que l'agitation des grains provienne de zones en mouvement, elle pénètre profondément dans les régions inactives, donnant ainsi naissance à une rhéologie non locale.

The full text of this article is available in PDF format.

Keywords : Slow granular flows, Rheology, Nonlocal models, Agitations

Mots-clés : Écoulements granulaires lents, Rhéologie, Modèles non locaux, Agitation granulaire

© 2014  Académie des sciences@@#104156@@
EM-CONSULTE.COM is registrered at the CNIL, déclaration n° 1286925.
As per the Law relating to information storage and personal integrity, you have the right to oppose (art 26 of that law), access (art 34 of that law) and rectify (art 36 of that law) your personal data. You may thus request that your data, should it be inaccurate, incomplete, unclear, outdated, not be used or stored, be corrected, clarified, updated or deleted.
Personal information regarding our website's visitors, including their identity, is confidential.
The owners of this website hereby guarantee to respect the legal confidentiality conditions, applicable in France, and not to disclose this data to third parties.
Article Outline