- Stokes stream function
In
fluid dynamics , the Stokes stream function is used to describe thestreamline s andflow velocity in a three-dimensionalincompressible flow withaxisymmetry . A surface with a constant value of the Stokes stream function encloses astreamtube , everywheretangential to the flow velocity vectors. Further, thevolume flux within this streamtube is constant, and all the streamlines of the flow are located on this surface. Thevelocity field associated with the Stokes stream function is solenoidal—it has zerodivergence . This stream function is named in honor ofGeorge Gabriel Stokes .Cylindrical coordinates
Consider a
cylindrical coordinate system ( "ρ" , "φ" , "z" ), with the "z"–axis the line around which the incompressible flow is axisymmetrical, "φ" theazimuthal angle and "ρ" the distance to the "z"–axis. Then the flow velocity components "uρ" and "uz" can be expressed in terms of the Stokes stream function "ψ" by: [Batchelor (1967), p. 78.]:
The azimuthal velocity component "uφ" does not depend on the stream function. Due to the axisymmetry, all three velocity components ( "uρ" , "uφ" , "uz" ) only depend on "ρ" and "z" and not on the azimuth "φ".
The volume flux, through the surface bounded by a constant value "ψ" of the Stokes stream function, is equal to "2π ψ".
pherical coordinates
In spherical coordinates ( "r" , "θ" , "φ" ), "r" is the
radial distance from the origin, "θ" is thezenith angle and "φ" is theazimuthal angle . In axisymmetric flow, with "θ" = 0 the rotational symmetry axis, the quantities describing the flow are again independent of the azimuth "φ". The flow velocity components "ur" and "uθ" are related to the Stokes stream function "ψ" through: [Batchelor (1967), p. 79.]:
Again, the azimuthal velocity component "uφ" is not a function of the Stokes stream function "ψ". The volume flux through a stream tube, bounded by a surface of constant "ψ", equals "2π ψ", as before.
Zero divergence
In cylindrical coordinates, the
divergence of the velocity field u becomes: [Batchelor (1967), p. 602.]:as expected for an incompressible flow.
And in spherical coordinates: [Batchelor (1967), p. 601.]
:
References
*cite book | first=G.K. | last=Batchelor | authorlink=George Batchelor | title=An Introduction to Fluid Dynamics | year=1967 | publisher=Cambridge University Press | isbn=0521663962
*cite book | first=H. | last=Lamb | authorlink=Horace Lamb | year=1994 | title=Hydrodynamics | publisher=Cambridge University Press | edition=6th edition| isbn=9780521458689 Originally published in 1879, the 6th extended edition appeared first in 1932.
*cite journal | first=G.G. | last=Stokes | authorlink=George Gabriel Stokes | year= 1842 | title= On the steady motion of incompressible fluids | journal= Transactions of the Cambridge Philosophical Society | volume= 7 | pages= 439–453
Reprinted in: cite book | first= G.G. | last=Stokes | year= 1880 | title= Mathematical and Physical Papers, Volume I | publisher= Cambridge University Press | pages= 1–16 | url= http://www.archive.org/details/mathphyspapers01stokrichNotes
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