Physics:Helmholtz minimum dissipation theorem
In fluid mechanics, Helmholtz minimum dissipation theorem (named after Hermann von Helmholtz who published it in 1868[1][2]) states that the steady Stokes flow motion of an incompressible fluid has the smallest rate of dissipation than any other incompressible motion with the same velocity on the boundary.[3][4] The theorem also has been studied by Diederik Korteweg in 1883[5] and by Lord Rayleigh in 1913.[6] This theorem is, in fact, true for any fluid motion where the nonlinear term of the incompressible Navier-Stokes equations can be neglected or equivalently when [math]\displaystyle{ \nabla\times\nabla\times\boldsymbol{\omega}=0 }[/math], where [math]\displaystyle{ \boldsymbol{\omega} }[/math] is the vorticity vector. For example, the theorem also applies to unidirectional flows such as Couette flow and Hagen–Poiseuille flow, where nonlinear terms disappear automatically.
Mathematical proof
Let [math]\displaystyle{ \mathbf{u},\ p }[/math] and [math]\displaystyle{ E=\frac{1}{2}(\nabla\mathbf{u}+(\nabla\mathbf{u})^T) }[/math] be the velocity, pressure and strain rate tensor of the Stokes flow and [math]\displaystyle{ \mathbf{u}',\ p' }[/math] and [math]\displaystyle{ E'=\frac{1}{2}(\nabla\mathbf{u}'+(\nabla\mathbf{u}')^T) }[/math] be the velocity, pressure and strain rate tensor of any other incompressible motion with [math]\displaystyle{ \mathbf{u}=\mathbf{u}' }[/math] on the boundary. Let [math]\displaystyle{ u_i }[/math] and [math]\displaystyle{ e_{ij} }[/math] be the representation of velocity and strain tensor in index notation, where the index runs from one to three.
Consider the following integral,
- [math]\displaystyle{ \begin{align} \int (e_{ij}'-e_{ij})e_{ij}\ dV &= \int \frac{\partial(u_i'-u_i)}{\partial x_j} e_{ij}\ dV \end{align} }[/math]
where in the above integral, only symmetrical part of the deformation tensor remains, because the contraction of symmetrical and antisymmetrical tensor is identically zero. Integration by parts gives
- [math]\displaystyle{ \int (e_{ij}'-e_{ij})e_{ij}\ dV = \int (u_i'-u_i)e_{ij} n_j\ dA - \frac{1}{2} \int (u_i'-u_i) (\nabla^2 u_i)\ dV. }[/math]
The first integral is zero because velocity at the boundaries of the two fields are equal. Now, for the second integral, since [math]\displaystyle{ u_i }[/math] satisfies the Stokes flow equation, i.e., [math]\displaystyle{ \mu\nabla^2 u_i = \nabla p }[/math], we can write
- [math]\displaystyle{ \int (e_{ij}'-e_{ij})e_{ij}\ dV = -\frac{1}{2\mu} \int (u_i'-u_i) \frac{\partial p}{\partial x_i}\ dV. }[/math]
Again doing an Integration by parts gives
- [math]\displaystyle{ \int (e_{ij}'-e_{ij})e_{ij}\ dV = -\frac{1}{2\mu} \int p(u_i'-u_i) n_i \ dA + \frac{1}{2\mu} \int p\frac{\partial(u_i'-u_i)}{\partial x_i}\ dV. }[/math]
The first integral is zero because velocities are equal and the second integral is zero because the flow in incompressible, i.e., [math]\displaystyle{ \nabla\cdot\mathbf{u}=\nabla\cdot\mathbf{u}'=0 }[/math]. Therefore we have the identity which says,
- [math]\displaystyle{ \int (e_{ij}'-e_{ij})e_{ij}\ dV = 0. }[/math]
The total rate of viscous dissipation energy over the whole volume of the field [math]\displaystyle{ \mathbf{u}' }[/math] is given by
- [math]\displaystyle{ D' = \int \Phi' dV = 2\mu\int e_{ij}'e_{ij}' \ dV = 2\mu\int [e_{ij}e_{ij} + e_{ij}'e_{ij}'- e_{ij}e_{ij}]\ dV }[/math]
and after a rearrangement using above identity, we get
- [math]\displaystyle{ D' = 2\mu \int [e_{ij}e_{ij} +(e_{ij}'-e_{ij})(e_{ij}'-e_{ij})]\ dV }[/math]
If [math]\displaystyle{ D }[/math] is the total rate of viscous dissipation energy over the whole volume of the field [math]\displaystyle{ \mathbf{u} }[/math], then we have
- [math]\displaystyle{ D' = D + 2\mu \int (e_{ij}'-e_{ij})(e_{ij}'-e_{ij})\ dV }[/math].
The second integral is non-negative and zero only if [math]\displaystyle{ e_{ij}=e_{ij}' }[/math], thus proving the theorem.
Poiseuille flow theorem
The Poiseuille flow theorem[7] is a consequence of the Helmholtz theorem states that The steady laminar flow of an incompressible viscous fluid down a straight pipe of arbitrary cross-section is characterized by the property that its energy dissipation is least among all laminar (or spatially periodic) flows down the pipe which have the same total flux.
References
- ↑ Helmholtz, H. (1868). Verh. naturhist.-med. Ver. Wiss. Abh, 1, 223.
- ↑ von Helmholtz, H. (1868). Zur Theorie der stationären Ströme in reibenden Flüssigkeiten. Verh. Naturh.-Med. Ver. Heidelb, 11, 223.
- ↑ Lamb, H. (1932). Hydrodynamics. Cambridge university press.
- ↑ Batchelor, G. K. (2000). An introduction to fluid dynamics. Cambridge university press.
- ↑ Korteweg, D. J. (1883). XVII. On a general theorem of the stability of the motion of a viscous fluid. The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science, 16(98), 112-118.
- ↑ Rayleigh, L. (1913). LXV. On the motion of a viscous fluid. The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science, 26(154), 776-786.
- ↑ Serrin, J. (1959). Mathematical principles of classical fluid mechanics. In Fluid Dynamics I/Strömungsmechanik I (pp. 125-263). Springer, Berlin, Heidelberg.
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