For a given re-entrant corner geometry, we describe a two parameter family of solutions for the local asymptotic behaviour of the flow and stress fields of UCM fluids. The two parameters used are the coefficients of the upstream wall shear rate and pressure gradient. In describing this parametric so
Re-entrant corner flows of UCM fluids: The natural stress basis
β Scribed by J.D. Evans
- Publisher
- Elsevier Science
- Year
- 2008
- Tongue
- English
- Weight
- 763 KB
- Volume
- 150
- Category
- Article
- ISSN
- 0377-0257
No coin nor oath required. For personal study only.
β¦ Synopsis
This paper continues the description of a two parameter family of solutions for the local asymptotic behaviour of UCM fluids at re-entrant corners. Here, the natural stress basis is used to re-derive the equations in the core flow and boundary layers, with full description of the scalings and matching being given. The parametric solution dependence is completed with numerical deteremination of the coefficient of the downstream wall shear rate. The flow structure implicitly assumes the absence of a separating streamline in the upstream region.
π SIMILAR VOLUMES
We revisit the situation of steady planar flow of Phan-Thien-Tanner (PTT) fluids around re-entrant corners of angles /Λwhere 1/2 β€ Λ< 1. The model is considered in the absence of a solvent viscosity, under which a class of self-similar solutions has been identified with stress singularities of O(r -
We consider the planar flow of Phan-Thien-Tanner (PTT) fluids around a re-entrant corner of angle Ο/Ξ± where Ξ± β [1/2, 1). The model is considered in the absence of a solvent viscosity and the flow situation assumes complete flow around the corner with the absence of a lip votex. The local asymptotic
We consider the Upper Convected Maxwell (UCM) limit of the Phan-Thien-Tanner (PTT) equations for steady planar flow around re-entrant corners. The PTT equations give the UCM equations in the limit of vanishing model parameter Γ, this dimensionless parameter being associated with the quadratic stress