The UMIST-N Near-Wall Treatment Applied to Periodic Channel Flow
The UMIST-N Near-Wall Treatment Applied to Periodic Channel Flow
The UMIST-N Near-Wall Treatment Applied to Periodic Channel Flow
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CHAPTER 1. INTRODUCTION & LITERATURE SURVEY 5<br />
1.2 Turbulence Models<br />
RANS models are based upon the idea of filtering turbulence from the gov-<br />
erning equations of a flow so that it may be treated separately. This is due<br />
<strong>to</strong> Reynolds [59]. In EVMs, the problem of knowing the effect of turbulence<br />
on the mean flow is made tractable by employing the idea of a turbulent<br />
viscosity, based on the work of Boussinesq [6]. Turbulent viscosity may be<br />
calculated in a number of different ways.<br />
<strong>The</strong> simplest approach is <strong>to</strong> specify the turbulent viscosity at a given location<br />
based on known local quantities. Models based on this approach are called<br />
‘algebraic models’. Taylor [80] and Prandtl [54] have proposed an algebraic<br />
model in which turbulent viscosity is calculated as a function of a length scale<br />
and a local mean velocity gradient. <strong>The</strong> length scale is specified as a function<br />
of wall-distance. Unfortunately, an appropriate length scale can be difficult<br />
<strong>to</strong> obtain in complex geometries. Another limitation of algebraic models is<br />
that the dependence of turbulent viscosity on a local mean velocity gradient<br />
is unrealistic in many types of flow.<br />
To remove the latter limitation of algebraic models, ‘one-equation’ models<br />
track an additional turbulent quantity through the solution of an additional<br />
transport equation. <strong>The</strong> most popular choice of the additional quantity is<br />
the turbulent kinetic energy per unit mass, k (usually referred <strong>to</strong> simply as<br />
turbulent kinetic energy). Prandtl [55] proposed this approach. Spalart et<br />
al. [73] have proposed directly solving a transport equation for turbulent<br />
viscosity. A limitation that is common <strong>to</strong> all one-equation models is that a<br />
length scale is still required <strong>to</strong> fully specify the modelled flow.