T - V,
where T is the kinetic energy density of the fluid, and V is the pressure of the fluid. The pressure acts as the potential energy density.
The viscosity of the fluid has to be zero. Otherwise, friction would drain energy, and the traditional lagrangian method would not work.
^ ^
| | flow of fluid
| |
Suppose that we have a nice smooth solution for the equations. Let us transform it infinitesimally, so that we make the "parcels" of fluid to bump into each other:
^ ^
\ /
/ \ "bumping" flows of fluid
\ /
/ \
The slight variation in the path of the parcels contributes negligibly to T, but the bumping contributes significantly to V.
We proved that the nice smooth solution is not a stationary point of the action?
This might be a negative solution to one of the Millennium Problems:
Our thought experiment also explains turbulence: the action seeks an extremal point, and makes the paths of fluid parcels meandering, so that they bump into each other.
Let us check if we really can modify the total, integrated pressure with this trick. Maybe the pressure of the flow decreases somewhere else, and compensates for the pressure in the bumps?
An incompressible fluid is very unnatural. Can we make a stable physical system if one can create pressure without expending energy? If not, then the Navier-Stokes equations might have no solutions, except in some trivial cases.
In our example, we have a uniform laminar flow, which we replace with a "bumping" flow. Does this mean that even trivial solutions of the equations are unstable if the fluid is incompressible?
Can we make a meandering flow without affecting the kinetic energy T much? Yes
Let us add walls like this to the laminar flow:
^ ^ ^
| | | flow out
/ \ / \
\ / \ / "meandering" walls
/ \ / \
\ / \ /
^ ^ ^
| | | flow in
Each wall guides the flow which is close to the wall, making the flow meandering.
We can imagine parcels of the fluid moving along the walls. The parcels bump to each other. Each bump involves an increased pressure.
If the walls differ from a vertical line by an angle ε, then the kinetic energy T may grow by ~ ε², but the pressure grows by ~ ε. We found an infinitesimal variation which changes the value of the action. The original laminar flow was not an extremal point of the action.
There is a problem, however. If the horizontal pressure is increased in the meandering zone, the zone will start to expand outward. Does this spoil the variation? It makes the end state different from the one we started from. The end state should stay the same in the variation.
Preventing the meandering flow from expanding: put it inside a pipe
If the flow is infinitely wide in the horizontal dimension, then the outward pressure would not be a problem. Another way is to enclose the flow into a pipe.
The Millennium Problem does not allow walls, though. It is stated in an infinite pool of water, filling the entire ℝ³.
Let us have an infinitelty rigid pipe in the fluid, preventing the fluid from spreading from the zone where we make the flow meandering.
meandering
flow
■ ^ ^ ■
■ / \ ■
■ \ / ■
■ / \ ■
solid solid
wall wall
Does the variation above really increase the pressure V, while the kinetic energy T stays essentially the same?
If the original configuration already contains pressure, what happens?
Pressure must be the same in all directions: this spoils our simple idea
The pressure cannot be just horizontal in an ideal fluid. The pressure has to be the same in all directions. This observation spoils our simple idea.
pipe
/ /
/ /
\ \ bend
\ \
^
\ flow
In the bend, a difference in the horizontal pressure must accelerate a fluid parcel to the right. But the average pressure in the bend must be the same as in the pipe overall. Otherwise, the fluid would slow down in the bend, and its density would grow. That is not allowed as the fluid is incompressible.
This means that our meandering flows are not able to change the average pressure of the flow. The action integral over the pressure V is unchanged.
Turbulence must be a second order phenomenon?
Suppose that the system looks for an extremal point of the action. The analysis above showed that the value of the action cannot change much if we add meandering. However, the action could change a little, and that may be enough to create turbulence.
Hypothesis. Adding turbulence at some length scale L optimizes the action. Adding it at ever shorter scales, L / 2ⁿ, will optimize the action further. The optimization will not stop at any length scale. There is no smooth solution for the Navier-Stokes equations, in most cases.
The potential is created by the motion: this explains turbulence?
Suppose that the potential V in the lagrangian density is an external potential, say, gravity:
T - V.
The orbit of an object in a newtonian gravity field is very regular, for example, an ellipse. It is the very opposite of the chaos of turbulence.
In the Navier-Stokes lagrangian density, the potential V is created by the flow itself, as it is the pressure. This opens the door for a chaotic process.
Adding viscosity creates turbulence
A large viscosity creates turbulence. What happens to our meandering flows if there is a large viscosity?
Viscosity means that there is a shear stress. The fluid is more like a solid substance then. The pressure still is the same in all directions, though.
The lagrangian density cannot be as simple as given above, if viscosity is present.
D'Alembert's paradox
D'Alembert's paradox states that, in the absence of viscosity, a laminar, time-independent, flow is possible, and there is no turbulence and no drag.
The pressure of the fluid depends on the speed of the fluid. In the diagram, the flow is symmetric on the left and on the right. Consequently, the pressure is the same on the left and on the right. The pressure does not exert any force on the circular cylinder, i.e., there is no drag.
The physicist Ludwig Prandtl suggested in 1904 that there is a "no slip" condition of the fluid on the surface. The viscosity of the fluid is large close to the surface, even if the viscosity would be close to zero in the bulk of the fluid. The hypothesis can explain many empirical phenomena.
From where does the energy for turbulence come?
Let us assume that the fluid has a zero viscosity and is incompressible. In the diagram above, the red cylinder is static. It cannot do any work.
Since the fluid is incompressible, the average horizontal speed component of the parcels of fluid must be constant. If the fluid arrives straight from the left, it cannot lose any of its original kinetic energy.
If there is turbulence on the right, then parcels have a vertical velocity component. They gained kinetic energy. From where did they obtain that energy? The explanation has to be that the pressure is larger on the left than on the right. A parcel slides down this pressure potential and gains kinetic energy.
Bernoulli's principle
For a time-independent (potential) flow, a larger velocity means a lower pressure.
Bernoulli's principle states that for a steady (= time-independent) flow with a zero viscosity, the energy of a parcel of fluid is constant. The pressure serves as the "potential" of the parcel.
Thus, the lagrangian density which we mentioned at the beginning of this blog post, only works for a time-independent flow.
Suppose that the flow is time-independent and we have a flow which is the stationary point of the action
∫ T - V dt,
where V is the pressure. For a time-independent flow, Bernoulli's principle holds. Let us assume that we "feed" the flow at a constant pressure p and kinetic energy density E. Then
T + V = E + p.
Is the stationary point also a stationary point of the action
∫ T dt?
For a time-dependent flow, the energy of a parcel is the kinetic energy plus its (very small) potential energy from compression. Maybe we can write a lagrangian density based on that?
*** WORK IN PROGRESS ***