TY - JOUR
T1 - Instability and freezing in a solidifying melt conduit
AU - Holmes-Cerfon, Miranda C.
AU - Whitehead, J. A.
N1 - Funding Information:
Support was received from the Geophysical Fluid Dynamics Program, which is supported by the Ocean Sciences Division of the National Science Foundation under Grant OCE-0325296 , and from the Oceanography Section of the Office of Naval Research under Grant N00014-07-1-0776 . The laboratory experiments were supported by the Deep Ocean Exploration Institute of W.H.O.I. M.C. Holmes-Cerfon would like to thank Lou Howard for many helpful conversations during the GFD summer program. We are also very grateful for the thorough help and comments of two anonymous referees.
PY - 2011/1/15
Y1 - 2011/1/15
N2 - Previous works have shown that when liquid flows in a pipe whose boundary temperature is below freezing, a tubular drainage conduit forms surrounded by solidified material that freezes shut under the appropriate combination of forcing conditions. We conduct laboratory experiments with wax in which the tube freezes shut below a certain value of flux from a pump. As the flux is gradually decreased to this value, the total pressure drop across the length of the tube first decreases to a minimum value and then rises before freezing. Previous theoretical models of a tube driven by a constant pressure drop suggest that once the pressure minimum is reached, the states for a lower flux should be unstable and the tube should therefore freeze-up. In our experiments, flux and pressure drop were coupled, and this motivates us to extend the theory for low Reynolds number flow through a tube with solidification to incorporate a simple pressure-dropflux relationship. Our model predicts a steady-state relationship between flux and pressure drop that has a minimum pressure as the flux is varied. The stability properties of these steady states depend on the boundary conditions: for a fixed flux, they are all stable, whereas for fixed pressure drop, only those with a flux larger than that at the pressure drop minimum are stable. For a mixed pressureflux condition, the stability threshold of the steady states lies between these two end members. This provides a possible mechanism for the experimental observations.
AB - Previous works have shown that when liquid flows in a pipe whose boundary temperature is below freezing, a tubular drainage conduit forms surrounded by solidified material that freezes shut under the appropriate combination of forcing conditions. We conduct laboratory experiments with wax in which the tube freezes shut below a certain value of flux from a pump. As the flux is gradually decreased to this value, the total pressure drop across the length of the tube first decreases to a minimum value and then rises before freezing. Previous theoretical models of a tube driven by a constant pressure drop suggest that once the pressure minimum is reached, the states for a lower flux should be unstable and the tube should therefore freeze-up. In our experiments, flux and pressure drop were coupled, and this motivates us to extend the theory for low Reynolds number flow through a tube with solidification to incorporate a simple pressure-dropflux relationship. Our model predicts a steady-state relationship between flux and pressure drop that has a minimum pressure as the flux is varied. The stability properties of these steady states depend on the boundary conditions: for a fixed flux, they are all stable, whereas for fixed pressure drop, only those with a flux larger than that at the pressure drop minimum are stable. For a mixed pressureflux condition, the stability threshold of the steady states lies between these two end members. This provides a possible mechanism for the experimental observations.
KW - Fluid dynamics
KW - Magma
KW - Melt conduits
KW - Solid/melt interface
KW - Stability analysis
KW - Viscous fluid
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U2 - 10.1016/j.physd.2010.10.009
DO - 10.1016/j.physd.2010.10.009
M3 - Article
AN - SCOPUS:78649726661
SN - 0167-2789
VL - 240
SP - 131
EP - 139
JO - Physica D: Nonlinear Phenomena
JF - Physica D: Nonlinear Phenomena
IS - 2
ER -