Editorial
Visco-plastic fluids: From Theory to Application

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    Bingham fluid as a kind of non-Newtonian fluid has attracted more and more interests to scientists and researchers (Frigaard and Nouar, 2003; Zhang, 2003; Osalusi et al., 2007; Firouzi and Hashemabadi, 2008; Staron et al., 2013; Liu and Liu, 2014). The Bingham fluids belong to viscous plastic fluids (Ancey et al., 2009; Chevalier et al., 2013; Chevalier and Talon, 2015) and exhibit a yield stress (Abdali et al., 1992; Li and Yu, 2010). Only after the applied stress exceeds the yield stress can Bingham fluids flow (Tichy, 1991).

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    The mixture motion and the settlement are described by constitutive law. Geophysical mass flows can be modelled by viscoplastic rheology [49–51,53]. Domnik et al. [24] proposed the pressure and rate-dependent Coulomb viscoplastic rheological model to describe the full dynamics of the rapid flows of granular materials down the channels impinging on rigid walls.

  • Viscoplastic Fluids from Theory to Application: 10 Years On

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    The past few years have seen the appearance of some excellent, up-to-date review articles [2,3] and a new book [4] on viscoplastic fluid mechanics. The work presented at the previous five VPF workshops has been published in a series of special issues of journals [5–9]. These, along with the present volume, provide a useful overview of the recent development of the field.

  • Debris flows: Experiments and modelling

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    It only depends weakly on the assumed constitutive law, but there is little experimental or theoretical evidence for a satisfactory description. Although field observations [11] have shown the presence of an almost entirely dry granular flow front, theoretical and laboratory modelling approaches have focused upon the fluid-filled core of the flow [12–14], which replicate bulk dynamics surprisingly well. But this approach cannot tell us about the peak velocities, impact pressures and flow heights that will occur within the highly energetic dry granular regions of the flow.

  • The mechanics of granitoid systems and maximum entropy production rates

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