Navier Stokes equations

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Governing equations

Transport equation for the momentum density (Navier-Stokes equations)

(1)\qquad
\varrho\,\frac{d\vec{v}}{dt}\,=\,\nabla\cdot\underline{\tau} + \vec{f}


where \vec{v}(x,z) and \vec{f}(x,z) are the velocity and a body force field, respectively. We use

(2)\qquad
\vec{v}=\left(\begin{matrix}u\\ w\end{matrix}\right),\qquad
\vec{f}=\left(\begin{matrix}f_1\\ f_2\end{matrix}\right)
\qquad\mbox{and}\qquad
\nabla=\left(\begin{matrix}\partial_x\\ \partial_z\end{matrix}\right).

In the following we will denote partial derivatives with respect to i either by \partial_i or simply by the subscript i. The body force may be potential, i.e. given by \vec{f}=-\nabla\phi. The stress tensor writes

(3)\qquad
\underline{\tau}\,=\,-p+\eta(\nabla\vec{v}+(\nabla\vec{v})^T).

where p(x,z) stands for the pressure field. The material derivative is defined by

(4)\qquad
\frac{d}{dt}\,=\,\frac{\partial}{\partial t}+(\vec{v}\cdot\nabla).

Boundary conditions

At a smooth solid substrate

For the velocity field at the substrate (z = 0) classically one assumes the no-slip and the no-penetration condition.

(5)\qquad
\vec{v}=0.


At a free surface

At the free surface (z = h(x)) one has the

kinematic condition (surface follows flow field)

(6)\qquad
w=\partial_th+u\partial_xh

and the force equilibrium

(7)\qquad
\underline{\tau}\cdot\vec{n}=-K\gamma\,\vec{n}\,+\,(\partial_s\gamma)\,\vec{t}

where the surface derivative is defined by \partial_s=\vec{t}\cdot\nabla and we assume that the ambient air does not transmit any force (\underline{\tau}_{air}=0). The term pL = − Kγ corresponds to the Laplace or curvature pressure whereas \partial_s\gamma results from the variation of the surface tension along the surface (resulting, for instance, from solutal or thermal Marangoni effects). The latter is modelled in the simplest case by a linear dependence of the surface tension on temperature; γ = γ0 + γT(T0T), where γ0 is the surface tension at the reference temperature T0and γT = dγ / dT.

(8)\qquad
\vec{n}=\frac{(-\partial_xh,1)}{\left(1+(\partial_xh)^2\right)^{1/2}},
\quad\vec{t}=\frac{(1,\partial_xh)}{\left(1+(\partial_xh)^2\right)^{1/2}},
\quad K=\frac{\partial_{xx}h}{\left(1+(\partial_xh)^2\right)^{3/2}}

are the normal vector, tangent vector and curvature of the surface, respectively.

The boundary condition (\ref{th-hddf5}) is of vectorial character, i.e.\ one can derive two scalar conditions by projecting it onto \vec{n} and \vec{t}, respectively.

(9)\qquad
\vec{t}:\quad \eta\,[(u_z+w_x)(1-h_x^2)+2(w_z-u_x)h_x]=\partial_s\gamma(1+h_x^2)
(10)\qquad
\vec{n}:\quad p+\frac{2\eta}{1+h_x^2}\left[-u_xh_x^2-w_z+h_x(u_z+w_x)\right]=-\frac{\gamma
h_{xx}}{(1+h_x^2)^{3/2}}


See Eq.(1)



References:

[1] Batchelor

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