Fluid Mechanics: 2D Laminar Flow

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SUMMARY

The discussion focuses on the analysis of two-dimensional incompressible laminar flow over a flat surface, specifically using the boundary layer approximation given by the equation u ≈ U(2*(y/δ) - 6*(y³/δ⁴) + y⁴/δ⁴), where δ = Cx¹/². Participants clarify the application of the continuity equation ∂u/∂x + ∂v/∂y = 0 and the necessity of including the term dδ/dx in the derivative calculations. The chain rule is confirmed as the method to derive this term, emphasizing its importance in fluid mechanics.

PREREQUISITES
  • Understanding of incompressible fluid dynamics
  • Familiarity with boundary layer theory
  • Knowledge of the continuity equation in fluid mechanics
  • Proficiency in applying the chain rule in calculus
NEXT STEPS
  • Study the derivation of the boundary layer equations in fluid mechanics
  • Learn about the implications of the continuity equation in two-dimensional flow
  • Explore the application of the chain rule in multivariable calculus
  • Investigate the effects of varying δ on laminar flow characteristics
USEFUL FOR

Students and professionals in mechanical engineering, particularly those specializing in fluid mechanics, as well as researchers analyzing laminar flow behavior in various applications.

jdawg
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Homework Statement


A reasonable approximation for the two-dimensional incompressible laminar boundary layer on the flat surface in Fig. P4.17 is

u ≈ U(2*(y/δ) - 6*(y34) + y44)

δ = Cx1/2 where C is a constant

y ≤ δ

Homework Equations

The Attempt at a Solution


Incompressible so density is constant, 2D flow so no z component, continuity equation reduces to
∂u/∂x + ∂v/∂y = 0For the x component, I got [ (-2y/δ2) + (6*y34) - (4*y45) ]

But there is supposed to be a dδ/dx term attached to each term. Where does this term come from? Is it some kind of chain rule thing? Thanks!
 
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jdawg said:
U(2*(y/δ) - 6*(y34) + y44)
I assume you mean 6(y33).
jdawg said:
Is it some kind of chain rule thing?
Yes. ∂/∂x of f(y, z) where z is a function of x is given by ∂f/∂z dz/dx.
 

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