Titlebook: Mechanics Down Under; Proceedings of the 2 James P. Denier,Matthew D. Finn Conference proceedings 2013 ? Springer Science+Business Media Do

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,Relaxation to Steady Vortical Flows – And Knots in the Quark-Gluon Plasma,eviewed, and compared with alternative artificial relaxation procedures that conserve the topology of the vorticity field. Attention is focussed first on axisymmetric vortex ring configurations, for which such relaxation techniques provide simple proofs of the existence of vortex rings of prescribed

畸形

EVICT

From Dry Granular Flows to Submarine Avalanches,nts a challenge due to the lack of constitutive laws able to describe the rich phenomenology observed. In a first part of the paper, we rapidly review the properties of dry granular flows and we discuss recent advances in our understanding of their rheological behaviour. In a second part we discuss

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Failure of Rocks in the Laboratory and in the Earth,ications and phenomena of societal interest. These include natural disasters, such as landslides, volcanic eruptions and earthquakes. Rocks are widely used for building materials, foundations, tunnels and underground facilities. Most of the world’s energy now, and for the foreseeable future, comes f

爵士樂

SUE

The Aerodynamics of Wind Turbines,dynamic research in wind energy. Next, we focus on some recent research results obtained by our wind energy group at Department of Mechanical Engineering at DTU. In particular, we show some new results on the classical problem of the ideal rotor and present a series of new results from an on-going r

ATP861

Cohesive-Zone Modeling of Adhesive Joints,esive, and an energy-based criterion using the toughness of the adhesive. In practice there are conditions under which the properties of a joint may be controlled by either one of these criteria, or by both. Cohesive-zone models have an advantage in that they incorporate both criteria simultaneously

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Surface Bubbles in Micro- and Nanofluidics,fashion. In addition, by further minaturizing the pits down to diameters of 100nm, Borkent et al. [4] could measure the pressure at which these bubbles start to nucleate, giving results in perfect agreement with the theory by Atchley and Prosperetti [10]. In contrast, so-called surface nanobubbles,

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Instabilities across the Scales: Simple Models for Shear Banding, Plate Subduction and Mantle Conve oriented with respect to the stress field. As coupled crust/mantle models become more sophisticated it is important to be able to use whichever failure model is appropriate to a given part of the system. We have therefore developed a way to represent Mohr-Coulomb failure within a mantle-convection

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