Parallel Large Eddy Simulation with UG

Andreas Hauser () and Gabriel Wittum ()
Additional contact information
Andreas Hauser: University of Heidelberg, Simulation in Technology, IWR
Gabriel Wittum: University of Heidelberg, Simulation in Technology, IWR

A chapter in High Performance Computing in Science and Engineering ’06, 2007, pp 269-278 from Springer

Abstract: 3 Conclusion and outlook The simulation of the fluid flow has been simulated on the levels l 2, l 3, l 4. The results on level l 2 and l 4 are plausible and suggest convergent behavior, whereas the results on l 3 does not fit in this sequence. The quantitative comparison along a line within the numerics show good agreement for all three levels. This can be explained with the fact, that the velocities in the middle of the mixer coincide in the cross section after the mixing element too. The ultimate validation with experiments show quite good agreement with respect to quality and quantity. Finally, as uniform refinement increases the complexity of the computation tremendously, effort in adaptive methods for turbulent flow has been invested already and should be applied to the static mixer soon.

Keywords: Large Eddy Simulation; Static Mixer; Direct Numerical Simulation; Axial Velocity; Coherent Structure (search for similar items in EconPapers)
Date: 2007
References: Add references at CitEc
Citations:

There are no downloads for this item, see the EconPapers FAQ for hints about obtaining it.

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:spr:sprchp:978-3-540-36183-1_19

Ordering information: This item can be ordered from
http://www.springer.com/9783540361831

DOI: 10.1007/978-3-540-36183-1_19

Access Statistics for this chapter

More chapters in Springer Books from Springer
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().