One set of models of this condition suffer from an over-prediction problem called the "stagnation point anomaly", which can be corrected for using the Kato-Laudner method. The k-epsilon and k-omega constructs are two-equation models of this phenomenon. Heat transfer under this condition can be approximated by the Dittus-Boelter equation. One equation describing materials under this condition uses a universal constant of 0.4 and is based on the first two derivatives of (*) velocity, and Prandtl found a similar logarithmic formula based on a model of momentum transfer. A characteristic feature of this condition disappears at sizes below the Kolmogorov limit. This condition is necessary to apply the Colebrook equation, and the presence of this phenomenon gives rise to the 1.75 term in the Ergun equation. Mixing-length and eddy viscosity models are used to describe, for 10 points, what regime of fluid flow that occurs at high Reynolds numbe
One set of models of this condition suffer from an over-prediction problem called the "stagnation point anomaly", which can be corrected for using the Kato-Laudner method. The k-epsilon and k-omega constructs are two-equation models of this phenomenon. Heat transfer under this condition can be approximated by the Dittus-Boelter equation. One equation describing materials under this condition uses a universal constant of 0.4 and is based on the first two derivatives of (*) velocity, and Prandtl found a similar logarithmic formula based on a model of momentum transfer. A characteristic feature of this condition disappears at sizes below the Kolmogorov limit. This condition is necessary to apply the Colebrook equation, and the presence of this phenomenon gives rise to the 1.75 term in the Ergun equation. Mixing-length and eddy viscosity models are used to describe, for 10 points, what regime of fluid flow that occurs at high Reynolds numbers?
One set of models of this condition suffer from an over-prediction problem called the "stagnation point anomaly", which can be corrected for using the Kato-Laudner method.
turbulence [or turbulent flow; prompt on “high Reynolds number” if anyone says something like that]