Numerical and experimental verification of a theoretical model of ripple formation in ice growth under supercooled water film flow
arXiv:1102.4890 · doi:10.1088/0169-5983/42/2/025508
Abstract
Little is known about morphological instability of a solidification front during the crystal growth of a thin film of flowing supercooled liquid with a free surface: for example, the ring-like ripples on the surface of icicles. The length scale of the ripples is nearly 1 cm. Two theoretical models for the ripple formation mechanism have been proposed. However, these models lead to quite different results because of differences in the boundary conditions at the solid-liquid interface and liquid-air surface. The validity of the assumption used in the two models is numerically investigated and some of the theoretical predictions are compared with experiments.
30 pages, 9 figures
References in corpus (1)
Cited by in corpus (5)
- Linear stability analysis of ice growth under supercooled water film driven by a laminar airflow
- On the origin and evolution of icicle ripples
- Morphological instability of the solid-liquid interface in crystal growth under supercooled liquid film flow and natural convection airflow
- Pattern of inclusions inside rippled icicles
- Roughness characteristics of an ice surface grown in the presence of a supercooled water film driven by gravity and wind drag