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Neutron radiography of an anisotropic drainage flow

Artem Skrypnik, Katie Cole, Tobias Lappan, Pablo R. Brito-Parada, Stephen J. Neethling, Pavel Trtik, Kerstin Eckert, and Sascha Heitkam
Phys. Rev. E 109, 014609 – Published 16 January 2024

Abstract

Liquid drainage through foam is dominated by gravity, capillary, and viscous forces. The liquid is conducted by an isotropic network of Plateau borders; however, imposed stress changes the alignment of the foam's structural elements. Previous numerical simulations predicted that a vertical drainage flow will be deflected horizontally if the foam is sheared. We investigated this phenomenon by measuring the distribution of the liquid fraction within a foam formed in a flat rectangular cell. The foam was subjected to shear stress under a forced liquid supply from the top of the cell. Neutron radiographies of unchanged and sheared foam were analyzed to extract measurements of the liquid fraction. Deflections in the distribution of the drainage liquid were detected and found to be positively correlated with increasing foam shear.

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  • Received 5 May 2023
  • Accepted 8 November 2023

DOI:https://doi.org/10.1103/PhysRevE.109.014609

©2024 American Physical Society

Physics Subject Headings (PhySH)

Polymers & Soft MatterFluid Dynamics

Authors & Affiliations

Artem Skrypnik1,*, Katie Cole2, Tobias Lappan3, Pablo R. Brito-Parada4, Stephen J. Neethling4, Pavel Trtik5, Kerstin Eckert1,3, and Sascha Heitkam1,3,†

  • 1Institute of Process Engineering and Environmental Technology, TU Dresden, 01062 Dresden, Germany
  • 2Department of Physics, University of Cape Town, 7700 Cape Town, South Africa
  • 3Institute of Fluid Dynamics, Helmholtz-Zentrum Dresden-Rossendorf, 01328 Dresden, Germany
  • 4Department of Earth Science and Engineering, Imperial College London, SW7 2AZ London, United Kingdom
  • 5Laboratory for Neutron Scattering and Imaging, Paul Scherrer Institut, 5232 Villigen, Switzerland

  • *artem.skrypnik@tu-dresden.de
  • sascha.heitkam@tu-dresen.de

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Issue

Vol. 109, Iss. 1 — January 2024

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