The friction factor is traditionally computed through Colebrook's equation or by using Moody's chart. However, these approaches have shown their limitations in getting accurate values for such factor. Different models to calculate the friction factor have been proposed, achieving different levels of certainty. In this paper, we revisit the distinct strategies used to estimate the friction factor and propose the use of a modified version of a model proposed by these authors. This model is based on the phenomenology of the flow as it transitions from laminar to turbulent flow conditions. Keywords Friction factor • Colebrook equation • Moody chart • Lambert W function • Artificial intelligence List of symbols ε Average projection of roughness, m ν Kinematic viscosity, m 2 /s ε/D Relative roughness f Friction factor Re Reynolds number and similar abbreviations do not use italics D Pipe diameter, m U Flow maximum velocity, m/s ū Flow mean velocity, m/s V* Shear force-velocity or friction velocity, m/s
A popular equation that is often employed to represent the relationship between the pressure loss and the fluid flow in fluidized or packed granular beds is the Ergun equation, which is an extension of Darcy’s law. In this paper, the method of Smoothed Particle Hydrodynamics (SPH) is used to numerically study the flow field across a rectangular channel partially filled with a porous layer both at the Representative Elementary Volume (REV) scale using the Ergun equation and at the pore scale. Since the flow field can be estimated at the REV scale with a much lower cost compared to the pore scale, it is important to evaluate how accurately the pore-scale results can be reproduced at the REV scale. The comparison between both scales is made in terms of the velocity profiles at the outlet of the rectangular channel and the pressure losses across the clear and porous zones for three different arrays of solid grains at the pore scale. The results show that minimum differences in the flow structure and velocity profiles between the REV and the pore scale always occur at intermediate values of the porosity (ϕ=0.44 and 0.55). As the porosity increases, the differences between the REV and the pore scale also increase. The details of the pressure losses are affected by the geometry of the porous medium. In particular, we find that the pressure profiles at the REV scale match those at the pore scale almost independently of the porosity only when the grains are uniformly distributed in a non-staggered square array.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.