Oldroyd B, and not A?

We examine Oldroyd's 1950 paper On the Formulation of Rheological Equations of State (Oldroyd, 1950) in which he introduced the upper and lower convected time-derivatives, along with the Oldroyd-A and Oldroyd-B model fluids. Those developments are placed in context of prior ideas and his own subsequent papers on constitutive equations. The choice between the A and B models is addressed by looking at micro-structural studies, finding that something in between is appropriate. Finally some refinements are discussed in terms of the elastic-dumbbell model.

Automated summary

The study examines Oldroyd's 1950 paper on rheological equations, introducing upper and lower convected time-derivatives, and the Oldroyd-A and Oldroyd-B model fluids. The choice between the A and B models is discussed based on micro-structural studies, suggesting something in between is appropriate. Finally, refinements are explored in terms of the elastic-dumbbell model.