Summary
In the absence of disturbances at the free surfaces, secondary flow due to elastic forces occurs in elastic liquids sheared in cone-and-plate rheometers but not in parallel-plate rheometers. In both types of apparatus an instability is observed. Using a theory based on a fracture mechanism, the critical normal stress differences for the onset of the instability can be correctly predicted for both types of apparatus. It is concluded that the fracture instability is a distinctly different effect from the secondary flow considered.
Similar content being viewed by others
References
Hutton, J. F., Nature200, 646 (1963). Proc. Roy. Soc. A287, 222 (1965).
Giesekus, H., Proc. Fourth Intern. Congr. Rheology, Providence 1963,1, 249 (1965); Rheol. Acta4, 85 (1965).
Oldroyd, J. G., Proc. Roy. Soc. A245, 278 (1958).
Rao, D. K. M., Proc. Indian Acad. Sci. A56, 198 (1962).
Lodge, A. S., Elastic Liquids (London 1964).
Walters, K., Private communication.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Hutton, J.F. Fracture and secondary flow of elastic liquids. Rheol Acta 8, 54–59 (1969). https://doi.org/10.1007/BF02321355
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF02321355