DefViscosity
Viscosity prevents the formation of discontinuities in real fluids. In general, (kinematic) viscosity is the diffusion of momentum. Commonly, the viscosity is related to temperature. Let μ be dynamic viscosity and ρ be density, we have ν=ρμ(m/s2)
DefBurgers’ Equation
For a given field u(x,t) and diffusion coefficient ν (i.e. viscosity in fluid mechanics), the Burger’s equation is defined as: ∂t∂u+u∂x∂u=ν∂x2∂2u
DefNewtonian Fluid
A newtonian fluid is a type of fluid such that stress is proportional to strain.
PropViscosity as Stickiness
The equation of motion of treating viscosity as stickiness between layers is given by: x¨=ν∂z2∂2u
DefNavier-Stokes Equations
The Navier-Stokes equations model essentially all fluid flows are defined by:
& \frac{D\vec{u}}{Dt}=-\frac{1}{\rho}\nabla P + \vec g + \nu \nabla^2\vec{u} \\
&\frac{D \rho}{Dt}+\rho \nabla \cdot \vec{u}=0
\end{aligned}$$
Specially, if $\nabla P = \vec g=0$ then the first equation reduces to the Burger's equation.
## Cascade to Turbulence
**Def** <i><u>Reynold’s Number</u></i>
Th Reynold’s number is a non-dimensional number that quantifies the relative strength of the viscous terms compared to the inertial, assuming a velocity scale of $u$ and a length scale of $L$:
$$ \text{Re}=\frac{uL}{\nu} $$
When Reynold’s number is considerably larger, the fluid behaves as an inviscid fluid except the boundaries. When it is order one, we have a fluid system which is influenced by the viscosity everywhere.
**Def** <i><u>Turbulence</u></i>
Turbulence is defined as continual cascade of instabilities at various scales. Turbulence is chaotic.
**Def** <i><u>Reynold’s Decomposition</u></i>
Let $\bar u = \frac{1}{T} \int_0^Tu \mathrm{d}t$ be the average velocity over time interval $T$, which is independent on $t$. Then define the following decomposition as Reynold’s decomposition:
$$ u^\prime = u-\bar u $$
**Prop** $\frac{1}{T} \int_0^Tu^\prime \mathrm{d}t=0$
**Def** <i><u>Turbulent Viscosity</u></i>
The turbulent or eddy viscosity $\nu_T \gg \nu$ is used to model the turbulence, which is known as large eddy simulation.
$$ \frac{D\bar{u}}{Dt}= \nabla \cdot ( (\nu_T+\nu) \nabla\bar{u} ) $$
where $\bar{u}$ is the mean velocity.