Beltrami flow
In fluid dynamics, Beltrami flows are flows in which the vorticity vector and the velocity vector are parallel to each other. In other words, Beltrami flow is a flow in which the Lamb vector is zero. It is named after the Italian mathematician Eugenio Beltrami due to his derivation of the Beltrami vector field, while initial developments in fluid dynamics were done by the Russian scientist Ippolit S. Gromeka in 1881.Gromeka, I. "Some cases of incompressible fluid motion." Scientific notes of the Kazan University (1881): 76–148.Truesdell, Clifford. The kinematics of vorticity. Vol. 954. Bloomington: Indiana University Press, 1954.
Description
Since the vorticity vector and the velocity vector are colinear to each other, we can write
:
where is some scalar function. One immediate consequence of Beltrami flow is that it can never be a planar or axisymmetric flow because in those flows, vorticity is always perpendicular to the velocity field. The other important consequence will be realized by looking at the incompressible vorticity equation
:
where is an external body forces such as gravitational field, electric field etc., and is the kinematic viscosity. Since and are parallel, the non-linear terms in the above equation are identically zero . Thus Beltrami flows satisfies the linear equation
:
When , the components of vorticity satisfies a simple heat equation.
Trkalian flow
Viktor Trkal considered the Beltrami flows without any external forces in 1919Trkal, V. "A remark on the hydrodynamics of viscous fluids." Cas. Pst. Mat, Fys 48 (1919): 302–311. for the scalar function , i.e.,
:
Introduce the following separation of variables
:
then the equation satisfied by becomes
:
The Chandrasekhar–Kendall functions satisfy this equation.
=Berker's solution=
Ratip Berker obtained the solution in Cartesian coordinates for in 1963,Berker, R. "Integration des equations du movement d'un fluide visqueux incompressible. Handbuch der Physik." (1963).高橋光一, & タカハシコウイチ. (2025). ナビエ-ストークス方程式の軸対称渦解 2. エネルギーの有限性について. 東北学院大学教養学部論集, 195, 31-47.
:
-\cos \frac{cx}{\sqrt 2}\,\sin \frac{cy}{\sqrt 2} \\ \sin \frac{cx}{\sqrt 2}\,\cos \frac{cy}{\sqrt 2} \\ \sqrt 2 \cos \frac{cx}{\sqrt 2}\,\cos \frac{cy}{\sqrt 2}
\end{bmatrix}.
Generalized Beltrami flow
The generalized Beltrami flow satisfies the conditionDrazin, Philip G., and Norman Riley. The Navier–Stokes equations: a classification of flows and exact solutions. No. 334. Cambridge University Press, 2006.
:
which is less restrictive than the Beltrami condition . Unlike the normal Beltrami flows, the generalized Beltrami flow can be studied for planar and axisymmetric flows.
=Steady planar flows=
For steady generalized Beltrami flow, we have and since it is also planar we have . Introduce the stream function
:
Integration of gives . So, complete solution is possible if it satisfies all the following three equations
:
A special case is considered when the flow field has uniform vorticity . Wang (1991)Wang, C. Y. 1991 Exact solutions of the steady-state Navier–Stokes equations, Annu. Rev. Fluid Mech. 23, 159–177. gave the generalized solution as
:
assuming a linear function for . Substituting this into the vorticity equation and introducing the separation of variables with the separating constant results in
:
The solution obtained for different choices of can be interpreted differently, for example, represents a flow downstream a uniform grid, represents a flow created by a stretching plate, represents a flow into a corner, represents an Asymptotic suction profile etc.
=Unsteady planar flows=
Here,
:
\nabla^2\psi = -\zeta,\quad
\frac{\partial \zeta}{\partial t} = \nabla^2\zeta,\quad
\zeta = - f(\psi, t)
.
==Taylor's decaying vortices==
G. I. Taylor gave the solution for a special case where , where is a constant in 1923.Taylor, G. I. "LXXV. On the decay of vortices in a viscous fluid." The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science 46.274 (1923): 671–674. He showed that the separation satisfies the equation and also
:
Taylor also considered an example, a decaying system of eddies rotating alternatively in opposite directions and arranged in a rectangular array
:
which satisfies the above equation with , where is the length of the square formed by an eddy. Therefore, this system of eddies decays as
:
O. Walsh generalized Taylor's eddy solution in 1992.Walsh, O. (1992). Eddy solutions of the Navier-Stokes equations. In The Navier-Stokes Equations II—Theory and Numerical Methods (pp. 306-309). Springer, Berlin, Heidelberg. Walsh's solution is of the form , where and
=Steady axisymmetric flows=
Here we have . Integration of gives and the three equations are
:
The first equation is the Hicks equation. Marris and Aswani (1977)Marris, A. W., and M. G. Aswani. "On the general impossibility of controllable axi-symmetric Navier–Stokes motions." Archive for Rational Mechanics and Analysis 63.2 (1977): 107–153. showed that the only possible solution is and the remaining equations reduce to
:
A simple set of solutions to the above equation is
:
represents a flow due to two opposing rotational stream on a parabolic surface, represents rotational flow on a plane wall, represents a flow ellipsoidal vortex (special case – Hill's spherical vortex), represents a type of toroidal vortex etc.
The homogeneous solution for as shown by BerkerBerker, R. "Integration des equations du movement d'un fluide visqueux incompressible. Handbuch der Physik." (1963).
:
where are the Bessel function of the first kind and Bessel function of the second kind respectively. A special case of the above solution is Poiseuille flow for cylindrical geometry with transpiration velocities on the walls. Chia-Shun Yih found a solution in 1958 for Poiseuille flow into a sink when .Yih, C. S. (1959). Two solutions for inviscid rotational flow with corner eddies. Journal of Fluid Mechanics, 5(1), 36-40.
Beltrami flow in fluid mechanics
{{Main|Beltrami vector field#Beltrami fields and fluid mechanics}}
Beltrami fields are a classical steady solution to the Euler equation. Beltrami fields play an important role in (ideal) fluid mechanics in equilibrium, as complexity is only expected for these fields.
See also
References
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