2009
DOI: 10.1016/j.jfluidstructs.2009.07.004
|View full text |Cite
|
Sign up to set email alerts
|

A vorticity formulation for computational fluid dynamic and aeroelastic analyses of viscous flows

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

0
4
0

Year Published

2011
2011
2018
2018

Publication Types

Select...
4

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(4 citation statements)
references
References 24 publications
0
4
0
Order By: Relevance
“…Specifically, to apply this method, one considers a potential flow and modifies its boundary condition, by replacing the potential-flow boundary condition ∂φ/∂n = χ B (see Eq. 15, where v = ∇φ), with 125where the equivalent source term, χ E , is given by 46 (126) with v α E denoting the contravariant components of v E , where v E is the "irrotational and solenoidal continuation" into the vortical region V ζ of the velocity v (which is irrotational and solenoidal outside the vortical region V ζ ).…”
Section: Relationship With the Lighthill Equivalent Source Methodsmentioning
confidence: 99%
See 2 more Smart Citations
“…Specifically, to apply this method, one considers a potential flow and modifies its boundary condition, by replacing the potential-flow boundary condition ∂φ/∂n = χ B (see Eq. 15, where v = ∇φ), with 125where the equivalent source term, χ E , is given by 46 (126) with v α E denoting the contravariant components of v E , where v E is the "irrotational and solenoidal continuation" into the vortical region V ζ of the velocity v (which is irrotational and solenoidal outside the vortical region V ζ ).…”
Section: Relationship With the Lighthill Equivalent Source Methodsmentioning
confidence: 99%
“…A primitive-variable boundary integral formulation unifying aeroacoustics and aerodynamics, and a natural velocity decomposition for vortical fields 46 In Eq. 126, we use a specific set of curvilinear coordinates ξ k (k = 1, 2, 3), with ξ 3 being the coordinate along the normal n, whereas ξ α (α = 1, 2) are curvilinear coordinates over S; in addition, ξ δ 3 denotes the value of ξ 3 just outside the boundary layer, J is the Jacobian of the transformation x = x(ξ k ), whereas a α = ∂x/∂ξ α (α = 1, 2) are the surface base vectors, which are such that dS = ||a 1 × a 2 || dξ 1 dξ 2 .…”
Section: Relationship With the Lighthill Equivalent Source Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The first term, v P (x, t), is irrotational and is referred to as the irrotational portion of the velocity, whereas the second one, w, is related to the vorticity ζ : [31][32][33][34]. This approach is of interest here because of its close relationship with the present one, where, as we will see, these problems are also avoided.…”
Section: Review Of Pertinent Workmentioning
confidence: 96%