Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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Chaparian, Emad

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University of Strathclyde

in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (13/13 displayed)

  • 2023Squeeze cementing of micro-annuli6citations
  • 2022Computational rheometry of yielding and viscoplastic flow in vane-and-cup rheometer fixtures12citations
  • 2022Flow onset for a single bubble in a yield-stress fluid16citations
  • 2021The first open channel for yield-stress fluids in porous media11citations
  • 2021Clouds of bubbles in a viscoplastic fluid7citations
  • 2020Yield-stress fluids in porous media39citations
  • 2020Stability of particles inside yield-stress fluid Poiseuille flows5citations
  • 2020Particle migration in channel flow of an elastoviscoplastic fluid20citations
  • 2020Computing the yield limit in three-dimensional flows of a yield stress fluid about a settling particle19citations
  • 2019An adaptive finite element method for elastoviscoplastic fluid flows28citations
  • 2018L-box - A tool for measuring the "yield stress"14citations
  • 2017Cloaking35citations
  • 2017Yield limit analysis of particle motion in a yield-stress fluid46citations

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Trudel, Elizabeth
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Izadi, Mahdi
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Frigaard, Ian
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Mckinley, Gareth H.
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Owens, Crystal E.
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Pourzahedi, Ali
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Frigaard, Ian A.
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Roustaei, Ali
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Tammisola, Outi
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Fraggedakis, Dimitrios
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Izbassarov, Daulet
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Vita, Francesco De
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Brandt, Luca
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Ardekani, Mehdi N.
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Iglesias, José A.
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Mercier, Gwenael
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Nasouri, Babak
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Co-Authors (by relevance)

  • Trudel, Elizabeth
  • Izadi, Mahdi
  • Frigaard, Ian
  • Mckinley, Gareth H.
  • Owens, Crystal E.
  • Pourzahedi, Ali
  • Frigaard, Ian A.
  • Roustaei, Ali
  • Tammisola, Outi
  • Fraggedakis, Dimitrios
  • Izbassarov, Daulet
  • Vita, Francesco De
  • Brandt, Luca
  • Ardekani, Mehdi N.
  • Iglesias, José A.
  • Mercier, Gwenael
  • Nasouri, Babak
OrganizationsLocationPeople

article

Stability of particles inside yield-stress fluid Poiseuille flows

  • Chaparian, Emad
  • Tammisola, Outi
Abstract

<p>The stability of neutrally and non-neutrally buoyant particles immersed in a plane Poiseuille flow of a yield-stress fluid (Bingham fluid) is addressed numerically. Particles being carried by the yield-stress fluid can behave in different ways: they might (i) migrate inside the yielded regions or (ii) be transported without any relative motion inside the unyielded region if the yield stress is large enough compared to the buoyancy stress and the other stresses acting on the particles. Knowing the static stability of particles inside a bath of quiescent yield-stress fluid (Chaparian &amp; Frigaard, J.A Fluid Mech., vol.A 819, 2017, pp.A 311-351), we analyse the latter behaviour when the yield-stress fluid Poiseuille flow is host to two-dimensional particles. Numerical experiments reveal that particles lose their stability (i.e. break the unyielded plug and sediment/migrate) with smaller buoyancy compared to the sedimentation inside a bath of quiescent yield-stress fluid, because of the inherent shear stress in the Poiseuille flow. The key parameter in interpreting the present results is the position of the particle relative to the position of the yield surface in the undisturbed flow (in the absence of any particle): the larger the portion of a particle located inside the undisturbed sheared regions, the more likely is the particle to be unstable. Yet, we find that the core unyielded plug can grow locally to some extent to contain the particles. This picture holds even for neutrally buoyant particles, although they are strictly stable when they are located wholly inside the undisturbed plug. We propose scalings for all cases.</p>

Topics
  • impedance spectroscopy
  • surface
  • experiment
  • two-dimensional