Taylor scraping flow polish, cream, butter, honey, etc.,), it is essential to consider this case. The analysis was carried out by J. Riedler and Wilhelm Schneider in 1983 and they were able to obtain self-similar solutions for power-law fluids satisfying the relation for the apparent viscosity where formula_41 and formula_42 are constants. The solution for the streamfunction of the flow created by the plate moving towards right is given by where and where formula_46 is the root of formula_47. It can be verified that this solution reduces to that of Taylor's for Newtonian fluids, i.e., when formula_48. Taylor scraping flow In fluid dynamics,
Connate fluids Connate fluids In geology and sedimentology, connate fluids are liquids that were trapped in the pores of sedimentary rocks as they were deposited. These liquids are largely composed of water, but also contain many mineral components as ions in solution. As rocks are buried, they undergo lithification and the connate fluids are usually expelled. If the escape route for these fluids is blocked, the pore fluid pressure can build up, leading to overpressure. An understanding of the geochemistry of connate fluids is important if the diagenesis of the rock is to be quantified. The solutes in the connate fluids often