Summary
The plane flow of ice over a bump as observed with the so-called Penelope ice viscometer has been calculated. The cavity which forms in the lee of the bump is included as an initial condition. The deformation of the ice is assumed to be the sum of the linear elasticity an the non-linear viscosity resulting from the Glen creep law.
A finite difference method based on orthogonal curvilinear co-ordinates is used to determine the stresses and deformation from unit ε 0 and σ 0, which are computed at the end of the procedure from the experimentally measured strains and torque. The model yields a very low Young’s modulus (E = 1250 bar) and a fluidity parameter B = T-3 y-1 = 0.079 bar-3 year-1. However, the fact that the outer ice remains bubbly makes the computed radial velocities unrealistic.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1980 Springer-Verlag, Berlin, Heidelberg
About this paper
Cite this paper
Brepson, R. (1980). Numerical Model of Penelope Ice Viscometer Flows. In: Tryde, P. (eds) Physics and Mechanics of Ice. International Union of Theoretical and Applied Mechanics. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-81434-1_3
Download citation
DOI: https://doi.org/10.1007/978-3-642-81434-1_3
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-81436-5
Online ISBN: 978-3-642-81434-1
eBook Packages: Springer Book Archive