Water flow down a porous channel (Navier-Stokes/Fluid dynamics)

Click For Summary
SUMMARY

The discussion focuses on the analysis of water flow down a porous channel using the Navier-Stokes equation. The x-component of the equation is given as ν(d²u/dy²) + v(du/dy) + G = 0, with the general solution verified as u = A - (G/v)y + Be^(-vy/ν). The boundary conditions are established as u(0) = 0 and u(H) = U, where U is the flow speed and H is the height of the channel. The challenge lies in eliminating the integration constants A, B, and G to arrive at the required solution u* = (1 - Re^(-R)y* - e^(-Ry*)) / (1 - (R + 1)e^(-R)), where R = vH/ν.

PREREQUISITES
  • Understanding of the Navier-Stokes equations in fluid dynamics
  • Familiarity with boundary conditions in differential equations
  • Knowledge of integration techniques for solving ordinary differential equations
  • Basic concepts of porous media flow
NEXT STEPS
  • Study the derivation and application of the Navier-Stokes equations in fluid dynamics
  • Learn about boundary layer theory and its implications in fluid flow
  • Explore methods for solving ordinary differential equations with boundary conditions
  • Investigate the principles of seepage flow in porous media
USEFUL FOR

Students and professionals in fluid dynamics, engineers working with porous media, and anyone involved in solving complex flow problems using the Navier-Stokes equations.

tome101
Messages
7
Reaction score
0

Homework Statement


Water flows down a channel whose floor is porous, so that water seeps out of the bottom of the channel at a speed v, where v is constant and much less than the flow speed, U, along the surface of the channel. The seepage rate is slow so that H may be regarded as constant.

The x−component of the Navier-Stokes equation for such a system is

[itex]\nu\frac{d^{2}u}{dy^{2}}+v\frac{du}{dy}+G=0[/itex]

where G is a constant.

Verify (i.e. no need to derive) that the general solution of this equation is

[itex]u=A-\frac{G}{v}y+Be^{-vy/\nu}[/itex]

where A and B are integration constants.
State clearly what the boundary conditions are that determine A, B and G, and verify that the required solution is:

[itex]u*=\frac{1-Re^{-R}y*-e^{-Ry*}}{1-(R+1)e^{-R}}[/itex]

where u = Uu*, y = Hy* and R = vH/[itex]\nu[/itex].

Homework Equations


u(0)=0

u(H)=U


The Attempt at a Solution


Ok, I managed the first part and have verified that the 2nd equation is indeed a solution of the first. However, I am having trouble removing the integration constants and G and rearranging to the required equation.

I know that at the top of the channel, u=U so u(H)=U. I'm also assuming that since v is 'much less' than the flow speed we can assum that at the bottom of the path the horizontal flow speed is equivalent to 0 (although I am less sure about this).

So that gives boundary conditions of:
u(H)=0
u(0)=0

Using u(0)=0 I can see that A+B=0

I can get an equation for U by using u(H).

However, I can't seem to find any useful way of rearranging these equations to a) remove A B and G or b) look anything like the final equation... I am also not 100% certain my boundary conditions are corect. Attached is a diagam of the problem. Any help would be greatly appreciated.

Thanks
 

Attachments

  • Untitled.jpg
    Untitled.jpg
    14.7 KB · Views: 515
Last edited:
Physics news on Phys.org
290 views and no-one has any thoughts on this? I'm still completely stumped! I've also just noticed i should say u(H)=U under the attempted solution
 
Last edited:
I'm not very familiar with fluid dynamics at all, but here are some thoughts:

Since you have three constants to eliminate, you'll need three equations. Your boundary conditions only give you two. You need to get one more constraint from somewhere.

The condition u(0)=0 is correct — you can see this by setting y*=0 in the provided solution — but your reason for it is wrong. It doesn't have to do with the seepage rate. It's the no-slip condition. The water doesn't slide along the channel floor.
 

Similar threads

  • · Replies 19 ·
Replies
19
Views
4K
  • · Replies 1 ·
Replies
1
Views
2K
  • · Replies 3 ·
Replies
3
Views
2K
  • · Replies 9 ·
Replies
9
Views
4K
  • · Replies 13 ·
Replies
13
Views
2K
  • · Replies 11 ·
Replies
11
Views
2K
  • · Replies 1 ·
Replies
1
Views
2K
  • · Replies 4 ·
Replies
4
Views
2K
  • · Replies 1 ·
Replies
1
Views
2K
  • · Replies 63 ·
3
Replies
63
Views
7K