A fluid of absolute viscosity of 0.045 Pa-s and sp gr of 0.91 flows over a flat plate. The velocity of fluid at 70mm height over the plate is 1.13m/s. Calculate the shear stress at the solid boundary and at points 20mm above the plate considering (a) linear velocity distribution, and (b) parabolic velocity distribution with vertex at point 70mm away from the surface.

Problem Statement

A fluid with an absolute viscosity of 0.045 Pa-s and a specific gravity of 0.91 flows over a flat plate. The velocity of the fluid at a height of 70 mm above the plate is 1.13 m/s. Calculate the shear stress:

  • At the solid boundary
  • At points 20 mm above the plate

Consider two cases:

  1. Linear velocity distribution
  2. Parabolic velocity distribution with a vertex at 70 mm above the surface

Solution

Given:

  • Absolute viscosity (μ) = 0.045 Pa-s
  • Specific gravity = 0.91
  • Velocity at 70 mm from the plate = 1.13 m/s

Case (a): Linear Velocity Distribution

Step 1: Velocity equation

u = ay

a = tanθ = u / y = 1.13 / 0.07 = 16.1

Therefore, u = 16.1y

Step 2: Velocity gradient (du/dy)

du/dy = 16.1

Step 3: Shear stress

τ = μ × du/dy

τ = 0.045 × 16.1 = 0.726 Pa (constant throughout)

Result for Case (a):

Shear stress is constant throughout the flow: 0.726 Pa.

Case (b): Parabolic Velocity Distribution

Step 1: Velocity equation

u = ay² + by + c

Boundary conditions:

  • At y = 0, u = 0 → c = 0
  • At y = 0.07 m, du/dy = 0 → 2a × 0.07 + b = 0 → b = -0.14a
  • At y = 0.07 m, u = 1.13 m/s

Substitute: 1.13 = a × (0.07)² – 0.14a × 0.07

Solving: a = -230.61, b = -0.14 × -230.61 = 32.29

Final equation: u = -230.61y² + 32.29y

Step 2: Velocity gradient (du/dy)

du/dy = -461.22y + 32.29

At y = 0:

du/dy = 32.29

At y = 0.02 m:

du/dy = -461.22 × 0.02 + 32.29 = 23.0656

Step 3: Shear stress

At y = 0:

τ = μ × du/dy = 0.045 × 32.29 = 1.453 Pa

At y = 0.02 m:

τ = μ × du/dy = 0.045 × 23.0656 = 1.038 Pa

Result for Case (b):

Shear stress at y = 0: 1.453 Pa

Shear stress at y = 0.02 m: 1.038 Pa

Explanation

In this problem, shear stress is calculated using the velocity gradient at different heights:

  1. Linear distribution: The velocity gradient is constant, so the shear stress remains the same at all points.
  2. Parabolic distribution: The velocity profile follows a parabola, leading to varying velocity gradients and shear stresses at different heights.

This illustrates how the velocity profile impacts shear stress in fluid flow over a flat plate.

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