Dislocation forest interactions: simulation and prediction
L.K. Wickham, K.W. Schwarz, et al.
MRS Proceedings 1999
It is shown that the superfluid turbulence arises as a convective, not an absolute, instability. A continuous source of macroscopic quantized vortices is therefore required, not only to initiate the turbulence, but also to keep the vortex tangle alive. It is demonstrated that a streamwise-pinned, remanent vortex at the channel inlet can act as the fluid dynamical analog of a phase-slip center, injecting vortex filaments into the flow at a steady rate. Several such vortex mills in tandem are sufficient to initiate and sustain the turbulent state. © 1990 The American Physical Society.
L.K. Wickham, K.W. Schwarz, et al.
MRS Proceedings 1999
H.D. Espinosa, M. Panico, et al.
International Journal of Plasticity
L.K. Wickham, K.W. Schwarz, et al.
Physical Review Letters
K.W. Schwarz
Modelling and Simulation in Materials Science and Engineering