Willingness to pay: Difference between revisions
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{{Multiple issues|unreferenced = November 2006|orphan = November 2009|context = May 2011|technical = May 2011| | |||
{{Underlinked|date=May 2013}} | |||
}} | |||
'''Streamline diffusion''', given an [[advection equation|advection]]-[[diffusion equation]], refers to all diffusion going on along the advection direction. | |||
==Explanation== | |||
If we take an advection equation, for simplicity of writing we have assumed <math>\nabla\cdot{\bold u}=0</math>, and <math>||{\bold u}||=1</math> | |||
:<math> | |||
\frac{\partial\psi}{\partial t} | |||
+{\bold u}\cdot\nabla\psi=0. | |||
</math> | |||
we may add a diffusion term, again for simplicty, we assume the diffusion to be constant over the entire field. | |||
:<math>D\nabla^2\psi</math>, | |||
Giving us an equation of the form: | |||
:<math> | |||
\frac{\partial\psi}{\partial t} | |||
+{\bold u}\cdot\nabla\psi | |||
+D\nabla^2\psi | |||
=0 | |||
</math> | |||
We may now rewrite the equation on the following form: | |||
:<math> | |||
\frac{\partial\psi}{\partial t} | |||
+{\bold u}\cdot \nabla\psi | |||
+{\bold u}({\bold u}\cdot D\nabla^2\psi) | |||
+(D\nabla^2\psi-{\bold u}({\bold u}\cdot D\nabla^2\psi)) | |||
=0 | |||
</math> | |||
The term below is called streamline diffusion. | |||
:<math>{\bold u}({\bold u}\cdot D\nabla^2\psi)</math> | |||
===Crosswind diffusion=== | |||
Any diffusion orthogonal to the streamline diffusion is called crosswind diffusion, for us this becomes the term: | |||
:<math> | |||
(D\nabla^2\psi-{\bold u}({\bold u}\cdot D\nabla^2\psi)) | |||
</math> | |||
[[Category:Fluid dynamics]] | |||
[[Category:Diffusion]] | |||
[[Category:Partial differential equations]] | |||
{{applied-math-stub}} |
Latest revision as of 21:04, 9 October 2013
Streamline diffusion, given an advection-diffusion equation, refers to all diffusion going on along the advection direction.
Explanation
If we take an advection equation, for simplicity of writing we have assumed , and
we may add a diffusion term, again for simplicty, we assume the diffusion to be constant over the entire field.
Giving us an equation of the form:
We may now rewrite the equation on the following form:
The term below is called streamline diffusion.
Crosswind diffusion
Any diffusion orthogonal to the streamline diffusion is called crosswind diffusion, for us this becomes the term: