Pressure variation in Navier-Stokes Equation

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Discussion Overview

The discussion revolves around the pressure variation in the Navier-Stokes equation for an incompressible Newtonian fluid sliding down an inclined plane. Participants explore the implications of hydrostatic pressure in a moving fluid and the role of shear stress in momentum conservation.

Discussion Character

  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant questions the application of hydrostatic pressure equations to a moving fluid, suggesting that shear stress should also influence pressure variation in the y-direction.
  • Another participant points out that shear stresses on the left and right faces of a fluid element cancel each other out, implying that only the shear stress on the bottom surface is relevant.
  • A participant requests clarification on the presence of two opposing shear stresses, asserting that the top surface experiences zero shear due to being a liquid-gas interface.
  • One participant presents a momentum shell balance approach, arguing that their results indicate pressure variation is shear dependent, contrary to hydrostatic assumptions.
  • Another participant emphasizes the need to consider the Cauchy stress relationship and the symmetry of the stress tensor in analyzing shear stresses.
  • There is a discussion about the definitions and roles of shear stresses in the context of the momentum balance, with some participants asserting that certain shear components should not be considered.

Areas of Agreement / Disagreement

Participants express differing views on the relevance of hydrostatic pressure versus shear stress in the momentum balance for the fluid system. The discussion remains unresolved, with multiple competing perspectives on how to approach the problem.

Contextual Notes

Participants highlight potential limitations in their assumptions, such as the treatment of shear stresses and the conditions under which hydrostatic pressure equations apply. The discussion also reflects varying interpretations of the Cauchy stress relationship and its implications for the problem at hand.

westmckay99
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Hello everyone,

I have a concern regarding the conservation of momentum for an incompressible Newtonian fluid with constant viscosity.

Say you have a volume of fluid sliding down an inclined plane with a velocity Vx with the perpendicular axis facing upward in the y-direction. When you try to solve the set of differential equations for Navier-Stokes in y, you end up with dp/dy=row*g, hence this illustrates the hydrostatic pressure variation. What doesn't make sense is how can a hydrostatic equation for a fluid at rest be applied to a fluid moving? When you derive the hydrostatic balance equation from a simple force balance on an element of fluid you only have 3 forces: Fdown(weight at top surface), Fup(weight at bottom surface), and Fdown(gravity force)... But in our inclined moving fluid system, we should have all the same weight Forces and the y-component of Fg AND also an extra Fdown(due to viscous transportation from the flow in the x-direction). Thus by virtue of this force balance, shouldn't the pressure variation in y be shear stress dependent and not simply a hydrostatic consideration?

I attached a diagram of the situation.

Thanks in advance!
 

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westmckay99 said:
Hello everyone,

I have a concern regarding the conservation of momentum for an incompressible Newtonian fluid with constant viscosity.

Say you have a volume of fluid sliding down an inclined plane with a velocity Vx with the perpendicular axis facing upward in the y-direction. When you try to solve the set of differential equations for Navier-Stokes in y, you end up with dp/dy=row*g, hence this illustrates the hydrostatic pressure variation. What doesn't make sense is how can a hydrostatic equation for a fluid at rest be applied to a fluid moving? When you derive the hydrostatic balance equation from a simple force balance on an element of fluid you only have 3 forces: Fdown(weight at top surface), Fup(weight at bottom surface), and Fdown(gravity force)... But in our inclined moving fluid system, we should have all the same weight Forces and the y-component of Fg AND also an extra Fdown(due to viscous transportation from the flow in the x-direction). Thus by virtue of this force balance, shouldn't the pressure variation in y be shear stress dependent and not simply a hydrostatic consideration?

I attached a diagram of the situation.

Thanks in advance!

If you are doing a differential force balance on the element you have shown, there are y-direction shear stresses on the left and the right faces of the element. One of these shear stresses is upward, and the other shear stress is downward. The two shear stresses are equal in magnitude, so they cancel.

I might also mention that, in your equation for dp/dy, there should be a negative sign and also a cosine theta.
 
Thanks for the reply! Could you please explain as to why there would be two shear stresses going in opposite directions here? The top surface is a liquid-gas interphase which experiences zero shear, only the bottom surface experiences shear stress due to the liquid-solid interphase boundary condition.

Thanks!
 
westmckay99 said:
Thanks for the reply! Could you please explain as to why there would be two shear stresses going in opposite directions here? The top surface is a liquid-gas interphase which experiences zero shear, only the bottom surface experiences shear stress due to the liquid-solid interphase boundary condition.

Thanks!

For a Newtonian fluid, σ_{xy}=σ_{yx}=η\left(\frac{\partial v_x}{\partial y}+\frac{\partial v_y}{\partial x}\right)

For your problem v_y=0 so,

σ_{xy}=σ_{yx}=η\left(\frac{\partial v_x}{\partial y}\right)

σxy is the shear stress on planes of constant y in the x direction, and σyx is the shear stress on planes of constant x in the y direction. The directionalities of the shear stresses on the left and right sides of your volume element follow from the Cauchy stress relationship.

Note that, because of the parabolic velocity profile, the shear stresses on the left and right faces of your volume element vary with y.

Chet
 
Chestermiller said:
For a Newtonian fluid, σ_{xy}=σ_{yx}=η\left(\frac{\partial v_x}{\partial y}+\frac{\partial v_y}{\partial x}\right)

For your problem v_y=0 so,

σ_{xy}=σ_{yx}=η\left(\frac{\partial v_x}{\partial y}\right)

σxy is the shear stress on planes of constant y in the x direction, and σyx is the shear stress on planes of constant x in the y direction. The directionalities of the shear stresses on the left and right sides of your volume element follow from the Cauchy stress relationship.

Note that, because of the parabolic velocity profile, the shear stresses on the left and right faces of your volume element vary with y.

Chet

Thanks again for the help. How is it that when I perform a momentum shell balance instead, I get different results: taking the +ve y direction to be pointing down instead

Momentum due to flow
@ x=0, (ρWΔyv_{x}v_{x})|_{x=0}
@ x=L, (ρWΔyv_{x}v_{x})|_{x=L}

Momentum due to viscous transport
@ y=y, (ζ_{yx}LW)|_{y=y}
@ y=y+Δy, (ζ_{yx}LW)|_{y=y+Δy}

Force due to pressure gradient
@ y=y, (pLW)|_{y=y}
@ y=y+Δy, -(pLW)|_{y=y+Δy}

Force due to gravity (generation)
(ρgcosθ)LWΔy

Assuming that we are at steady state (sum of forces equal to zero, no time accumulation) and assume fully developped flow ( v_{x=0}=v_{x=L}, momentum due to flow is zero), then

(ζ_{yx}LW)|_{y=y} - (ζ_{yx}LW)|_{y=y+Δy} + (pLW)|_{y=y} - (pLW)|_{y=y+Δy} + (ρgcosθ)LWΔy = 0

---divide by LWΔy---

\left(\frac{(ζ_{yx})|_{y=y} - (ζ_{yx})|_{y=y+Δy}}{Δy}\right) +\left(\frac{(p)|_{y=y} - (p)|_{y=y+Δy}}{Δy}\right) + (ρgcosθ) = 0

---taking the limit as Δy→0 and rearraging the equation---


\left(\frac{dζ_{yx}}{dy}\right) + \left(\frac{dp}{dy}\right) = - ρgcosθ

This shows that \left(\frac{dp}{dy}\right) is shear dependent, does it not?
 
ζxyLW is a force pointing in the x direction, so it should not be included in the y momentum balance. You need to look up the cauchy stress relationship, relating the stress vector acting on a surface of arbitrary orientation to the stress tensor and to a normal drawn to that surface. For a surface of constant y with a normal pointing in the +y direction, the stress vector is given by σyyiyxyix.
 
ζxy? I used ζyx as the shear stress pointing in the y direction due to flow in the x direction. Since there is no flow in y, shouldn't ζxy=0?
 
westmckay99 said:
ζxy? I used ζyx as the shear stress pointing in the y direction due to flow in the x direction. Since there is no flow in y, shouldn't ζxy=0?

No, it is not equal to zero because of the equation for the shear stresses I gave in post #4. The stress tensor is symmetric, so the xy component is equal to the yx component.

As you know, a shear stress, by definition is the component of the total stress vector on a surface which acts in the direction tangent to the surface. In terms of your control volume, it acts on the surfaces of constant y (top and bottom) in the x direction, and on the surfaces of constant x (left and right) in the y direction. If you include the shear stresses on the left and right faces of your control volume in the force balance in the y-direction, you will find that they exactly cancel, since the shear stress does not change with x, and the shear stress on one of the faces is directed upward, while the shear stress on the other face is directed downward. So the only shear stresses that matter are the ones on surfaces of constant y, and these are part of the x direction force balance.

Chet
 

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