If the velocity distribution law in a laminar boundary layer over a flat plate is assumed to be of the form u = ay + by³, determine the velocity distribution law.

Fluid Mechanics Problem Solution

Problem Statement

If the velocity distribution law in a laminar boundary layer over a flat plate is assumed to be of the form u = ay + by³, determine the velocity distribution law.

Given Data

Velocity Form u = ay + by³
Boundary Condition 1 At y = 0, u = 0
Boundary Condition 2 At y = δ, u = U
Boundary Condition 3 At y = δ, du/dy = 0

Solution Approach

To determine the velocity distribution law, we need to find the values of constants a and b by applying the given boundary conditions to the velocity profile equation u = ay + by³.

Calculations

Application of Boundary Conditions

Step 1: Apply the first boundary condition: At y = 0, u = 0

u = a(0) + b(0)³ = 0

This condition is automatically satisfied for any values of a and b.

Step 2: Apply the second boundary condition: At y = δ, u = U

U = aδ + bδ³

This gives us our first equation relating a and b.

Step 3: Apply the third boundary condition: At y = δ, du/dy = 0

du/dy = a + 3by²
At y = δ: a + 3bδ² = 0
Therefore: a = -3bδ²

Step 4: Substitute the expression for a into the equation from Step 2

U = -3bδ² · δ + bδ³
U = -3bδ³ + bδ³
U = -2bδ³
Solving for b: b = -U/(2δ³)

Step 5: Substitute the value of b back to find a

a = -3bδ² = -3(-U/(2δ³)) · δ² = 3U/(2δ)

Step 6: Substitute a and b into the original velocity equation

u = ay + by³
u = (3U/(2δ))y + (-U/(2δ³))y³
u = (3U/(2δ))y – (U/(2δ³))y³

Step 7: Express the velocity profile in non-dimensional form

u/U = (3/2)(y/δ) – (1/2)(y/δ)³

Velocity Distribution Law: u/U = (3/2)(y/δ) – (1/2)(y/δ)³

Detailed Explanation

Physical Significance of the Velocity Profile

The derived velocity profile u/U = (3/2)(y/δ) – (1/2)(y/δ)³ represents how the fluid velocity varies from the flat plate surface (y = 0) to the edge of the boundary layer (y = δ). This profile satisfies three essential boundary conditions:

  • No-slip condition at the wall: At y = 0, u = 0 (fluid velocity at the surface is zero)
  • Matching with free stream: At y = δ, u = U (velocity at the edge of the boundary layer equals the free stream velocity)
  • Smooth transition to free stream: At y = δ, du/dy = 0 (velocity gradient is zero at the edge of the boundary layer)

Properties of the Velocity Profile

The cubic velocity profile derived here has several important properties:

  • It follows a cubic relationship rather than the linear profile assumed in simpler models
  • Near the wall (small y), the profile is approximately linear: u ≈ (3U/2δ)y
  • As y increases, the cubic term becomes more significant, causing the velocity to level off
  • The maximum slope (maximum shear stress) occurs at the wall (y = 0)

Boundary Layer Theory Context

In boundary layer theory, we often use polynomial approximations to represent velocity profiles. The cubic profile derived here is a more refined approximation compared to simpler models like linear or quadratic profiles. It captures the essential physics of the boundary layer flow while maintaining mathematical simplicity.

Engineering Applications

Understanding the velocity distribution in a boundary layer is critical for:

  • Calculating skin friction drag on surfaces
  • Predicting heat transfer rates near surfaces
  • Designing more efficient airfoils and hydrofoils
  • Analyzing momentum transfer in fluid flows
  • Predicting separation points in adverse pressure gradients

Comparison with Other Models

This cubic model provides a good approximation for laminar boundary layers. However, it’s worth noting that:

  • For more accurate representations, higher-order polynomials or other mathematical forms might be used
  • The Blasius solution provides an exact solution for laminar boundary layers on flat plates
  • For turbulent boundary layers, different models like the power-law or logarithmic profiles are more appropriate

The derived profile u/U = (3/2)(y/δ) – (1/2)(y/δ)³ balances mathematical simplicity with physical accuracy, making it useful for both educational purposes and preliminary engineering calculations.

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