Correction: Steady shearing flows of deformable, inelastic spheres

Spectral analysis shows that the physi- cal evolution on the 4th track is a continuation of the flaring branch which we previously proposed consists of unstable nuclear burning of

In this graph (Fig. 37) it can be seen that the Volumetric Mass Transfer Coefficient KLa and the Standard Oxygen Transfer Rate increase by increasing both air velocity (parallel

Figura B.8: Andamento del livello z - variazione ampiezza coseno (modello con disponibilità del sedimento e incremento del medio mare). Figura B.9: Andamento del tasso di erosione

In order to stop, retain, dissipate or deflect debris flow events, different mitigation structures can be built; within this context, large or small scale experimental

Using accelerometers for velocity estimation, no model parameter is needed if we use a kinematic model relating to the position and use the acceleration measurement as input to set up

The interannual variability of the Indian Ocean (IO), with a particular focus on the effect of the South Tropical Atlantic (STA) teleconnection is investigated using both Regional

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It is recent news that the “New Guidelines for internal architectures in schools” (Italian Ministerial Decree April 11 th 2013) have been approved, whose inspiration is drawn from