Search the courses, subjects, tracks, games and features, or jump straight to a page.
Learn it your way
A short class with Sarah and her students. The other ways are under More.
Sign up free to listen. Transcripts are free to read.
Today, we will explore how shear stress operates in turbulent flow. Let's start with the basic equation τ = ρu*², where τ is the shear stress.
Can you explain what u* is?
Great question! u* is known as the friction velocity, which helps bridge the relationship between shear stress and velocity. It's often calculated as u* = √(τ₀/ρ).
And what does the ρ stand for?
ρ is the fluid density, and understanding this helps in determining how shear stress is proportional to the velocity squares. This will aid us in our later calculations.
Let’s discuss how we derive the velocity profile using boundary conditions. We'll use the fact that at the wall (y=R), the velocity is at its maximum.
So, if I understand correctly, u at the wall is equal to u_max?
Exactly! As we set u at y = R equal to u_max, we can write our equations to express C, which allows us to derive the velocity profile.
What's the form of the velocity profile?
It leads us to a logarithmic profile: u = u_max - 2.5u* ln(R/y). This is crucial in determining how flow behaves near a boundary.
Now we'll tackle a practical problem on shear stress using water flow through a pipe. Can anyone tell me the first step?
We need to identify our given values, like the diameter and velocity at specific points.
Correct! For this problem, we have a diameter of 0.1m and velocities at specified points. Write these down as it helps set the stage for our calculations.
Once we have those, how do we find the shear stress at the wall?
We use the equation for velocity defect and the shear stress formula τ₀ = ρu*² to get our result. Let’s work through the calculation for clarity.
Now let's look at the types of boundary layers—viscous, buffer, overlap, and turbulent layers. Who can explain one of them?
The viscous sublayer is where the velocity profile is almost linear, right?
Exactly! As we move away from the wall, turbulent effects become more pronounced in the layers like the overlap layer.
And how does this relate to rough and smooth boundaries?
Great query! If the irregularities on the surface are larger than the viscous sublayer, we consider the boundary to be rough. We'll dive deeper into that next.
Let’s finalize our understanding by differentiating between rough and smooth boundaries. Who can recall the metrics to evaluate them?
Nikuradse’s criteria for k/delta as less than 0.25 means it's smooth.
Excellent! And when it exceeds 6, we know it’s rough. Understanding these characteristics is crucial for application in fluid mechanics.
What about the transitional boundaries?
Transitional boundaries occur between 0.25 and 6. Remembering this helps in categorizing flows correctly.
A measure of the force exerted parallel to a surface per unit area.
A key scale used in fluid dynamics that relates to shear stress and flow characteristics.
The proximity zone adjacent to a wall where viscous effects dominate.
The farthest flow area from a wall where turbulence presents distinct flow attributes.
A description of how velocity varies logarithmically with height in turbulent flow situations.
When fluid flows with force so grand, shear stress gives us a helping hand.
Imagine a river with smooth stones; the water flows easily. But on a rocky bed, the flow is chaos. This story illustrates how smooth versus rough boundaries affect flow.
Remember the word 'SLAP' for shear, laminar, acceleration, and profile.
Use 'BOLT' to remember Boundaries, Overlap, Laminar, and Turbulent flow characteristics.
Term
What is shear stress?
Click to flip
Term
Define friction velocity.
Click to flip
Term
What is the logarithmic velocity profile?
Click to flip
Term
What does k represent in boundary layer analysis?
Click to flip
The force per unit area exerted parallel to the surface of a material.
A velocity scale in boundary layer theory that relates shear stress and velocity.
The thin layer closest to the wall where the flow is dominated by viscous effects, and the velocity profile is nearly linear.
The layer farthest from the wall where turbulence dominates the flow characteristics.
The region next to a surface where the effects of the surface affect the flow of the fluid.
A velocity profile characterized by a logarithmic dependence on distance from the wall, commonly seen in turbulent flow.
A boundary regime where the surface roughness height is between smooth and rough limits.
A criterion for defining surface roughness based on the ratio of surface irregularity height to the thickness of the viscous boundary layer.
This section discusses the integration of shear stress equations in fluid dynamics, focusing on turbulent flow and its boundary conditions.
The section explains the derivation of the logarithmic velocity profile in turbulent flow using shear stress equations and boundary conditions. It covers important fluid dynamics concepts including the presentation of laminar and turbulent flows, calculation of shear stress at pipe walls, and discussions of boundary layer properties.
In this section, we begin with the integration of shear stress equations within the context of turbulent fluid flow. Specifically, it discusses the assumption that for small values of y, shear stress at the wall, denoted as τ₀, can be taken as constant. By substituting τ as τ₀ in the derived equations, we can express the velocity gradient and derive useful equations that relate flow characteristics. A key focus is the derivation of the logarithmic velocity profile based on the Prandtl mixing length theory. The different characteristics of laminar versus turbulent flow are highlighted, and we explore the implications of boundary conditions on these profiles. The section also addresses practical applications, such as determining shear stress with worked examples that contextualize theoretical concepts in real-world scenarios. Ultimately, this understanding aids in both the theoretical formulation and practical calculations associated with turbulent flow and boundary layers.