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Discretization of the diffusion term

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Old   August 29, 2017, 21:16
Default Discretization of the diffusion term
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For incompressible NS equation in the finite volume discretization on a staggered grid, I have encountered a doubt.

We can put the diffusive term together with the advection term by factoring out gradient, for instance for x-direction for one term as below:
\frac{\partial }{\partial x}\left ( u^2-2 \mu \frac{\partial u}{\partial x} \right )

I am fine with the way to discretize the second term in staggered grid but for the first term in the code that I see someone has discretized the first term as
\frac{u^2_{i+1,j}-u^2_{i-1,j}}{2\Delta x }

Why is this correct? Even if it is the central difference, shouldn't it also include u_{ij}?
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Old   August 29, 2017, 21:29
Default Diffusion
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The finite difference discretization below ensures proper conservation.
\frac{u_{i+1}^{2} - u_{i-1}^{2}}{2 \Delta x}

The advection term of the form
u_{i} \frac{u_{i+1} - u_{i-1}}{2 \Delta x}

is not conservative and can lead to the numerical solution undershooting. As a side note, central differencing like that of the advection term can lead spurious oscillations. QUICK scheme or a stable advection scheme (ENO, WENO) can remedy such a problem.
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Old   August 29, 2017, 21:36
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So you mean all is good with the conservative form of discretization? And no oscillations occur?
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Old   August 29, 2017, 22:02
Default Conservative schemes
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Yes, you will want your scheme to be conservative. In terms of your second question, spurious oscillations can occur regardless if your scheme is conservative or not. A simple 1D example would be looking at the convection-diffusion equation and adjust the peclet number. You will find that upwind differencing will perform better than central differencing.
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Old   August 30, 2017, 03:59
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I agree, consider the Burgers equation in divergence and non-divergence (quasi-linear) form:

du/dt + d(u^2/2)/dx=d(mu*du/dx)/dx (divergence form)

du/dt + u*du/dx=mu*d2u/dx^2 (quasi linear)

No difference exists for the staggered or non staggered grid since the only involved variable is u.
Discretize with second order central difference a see what happens. The appearence of u(i,j) in the convective term:

d(u^2/2)/dx -> (u(i+1/2)^2-u(i-1/2)^2)/2/h
du/dx -> (u(i+1/2)-u(i-1/2))/h

Now you have two chance:
1) linear interpolation for u on the half-nodes
2) linear interpolation for u^2 on the half nodes

The first choice is congruent to a linear reconstruction of the flux function, the second one introduces aliasing in the terms.
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Old   August 30, 2017, 10:41
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Quote:
Originally Posted by mseka View Post
So you mean all is good with the conservative form of discretization? And no oscillations occur?
numerical oscillations are due to the lack of monotonicity of the scheme... Godunov theores states that monotonic linear scheme can be only first order accurate. Have also a look to the examples in the book of Peric & Ferziger
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