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Welcome everyone! Today, we are diving into the fascinating concept of eddy viscosity. Can anyone tell me what they think viscosity means in the context of fluid flow?
I think it refers to how thick a fluid is, or how easily it flows?
Exactly! Viscosity is a measure of a fluid's resistance to flow. In turbulent flow, we must also consider something called eddy viscosity. Can someone explain how this might differ from dynamic viscosity?
Is it because eddy viscosity is related to the turbulence in the fluid?
Yes, great point! Eddy viscosity captures the effects of turbulence on shear stress. So, when we talk about shear stress in turbulent flow, it’s not just about viscosity. Do you remember how shear stress was expressed in laminar flow?
It was just the dynamic viscosity times the velocity gradient, right?
Right! So in turbulent flow, we have a similar expression, but we add the component of eddy viscosity. Keep that in mind as we move forward.
Now that we've established what eddy viscosity is, let’s look at Reynolds shear stress. Does anyone know what this term describes?
I think it's the shear stress caused by fluctuations in the velocity components?
Correct! Reynolds shear stress is defined by the product of fluctuating velocity components, and it's vital to understand turbulent shear stress in fluid dynamics.
So, how is this different from regular shear stress?
Great question! Regular shear stress, in laminar flow, comes solely from the viscosity, while Reynolds shear stress incorporates turbulence effects, leading to a more complex understanding of fluid behavior.
Let’s talk about Prandtl's mixing length theory now. Who can summarize what mixing length is?
Isn't it the distance over which fluid particles mix with each other?
Exactly! The mixing length helps relate turbulent shear stress back to measurable quantities. So how does this relate to average velocity gradients?
I remember that it relates to how fluid layers interact within a turbulent flow?
Precisely! Prandtl argued that we can express the turbulent shear stress in terms of mixing length and the velocity gradient. This is a foundational concept in hydraulic engineering.
As we conclude this section, let’s consider how eddy viscosity and the mixing length theory apply in real-world scenarios. Can anyone think of an example?
I think about water flowing in a river—it's definitely turbulent and affects how we measure flow rates.
Exactly—the principles we discussed are essential for accurately predicting flow behavior in such contexts. Understanding turbulent shear stress will inform the design of efficient hydraulic structures.
So, when we design these structures, we should always consider both viscosity and turbulence?
Yes! That’s the takeaway. The interaction between eddy viscosity and turbulent shear stress is crucial for effective engineering solutions.
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In turbulent flows, shear stress is influenced not only by dynamic viscosity but also by turbulence-related forces, which can be quantified using the concept of eddy viscosity. This section delves into the derivation of shear stress forms from Boussinesq's model, the relationship of turbulent shear stress to Reynolds stress, and Prandtl's mixing length theory.
Eddy viscosity is an important concept in hydraulic engineering and fluid dynamics relevant to turbulent flow. Unlike laminar flow, where the shear stress is purely due to the fluid's dynamic viscosity (µ), turbulent flow incorporates additional shear stress components due to turbulence, leading to a higher total shear stress. Boussinesq's model introduces eddy viscosity (η) as a critical parameter, defined similarly to dynamic viscosity but dependent on flow conditions rather than just fluid characteristics.
Understanding eddy viscosity and turbulent shear stress is critical for applications in hydraulic engineering and designing efficient systems for fluid flow processes.
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In turbulent flow, there is an additional component of shear stress that happens because of the turbulence in the flow. Therefore, the shear stress in total is much larger than in viscous flow.
Eddy viscosity refers to the additional shear stress created by turbulence in a fluid flow, which is not present in laminar flow. In laminar flow, the shear stress is primarily due to the viscous properties of the fluid. However, in turbulent flow, due to chaotic fluctuations and mixing of fluid particles, there is an increase in shear stress. This leads to a higher total shear stress compared to that in laminar conditions, making the analysis of turbulent flows more complex.
Consider a calm river where the water flows smoothly (laminar flow) compared to a turbulent river section filled with rapids. In the calm section, the water flows steadily and evenly, resulting in lower shear stress. In contrast, in the rapids, the chaotic movement of water increases the shear stress due to turbulence, similar to how eddies form in a turbulent flow.
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Eddy viscosity is represented by a new coefficient of viscosity, denoted as eta (η), which is different from the dynamic viscosity (μ) of fluids.
Eddy viscosity quantifies the effect of turbulence on the flow properties of a fluid. It is not a fixed property of the fluid; instead, it varies depending on flow conditions. Unlike the dynamic viscosity, which is a characteristic of the fluid itself, eddy viscosity changes with the flow's velocity and distance from the wall. This variability is crucial in understanding turbulent flows in engineering applications.
Think of a stirred pot of soup versus a pot left still. In the stirred pot, the motion creates eddies and turbulence, while the still soup simply flows without mixing. The dynamic viscosity of the soup remains unchanged whether stirred or still, but the eddies formed when stirring affect how the soup mixes, illustrating how eddy viscosity works in a real-world scenario.
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In laminar flow, the value of eta is effectively zero, as it is related to turbulent viscosity, while the viscosity mu for laminar flow is typically around 10^(-3) Pascal seconds.
In laminar flow, the fluid particles move in parallel layers without disruption, making the contribution to shear stress solely dependent on classic viscosity (μ). In contrast, when considering turbulent flow, the turbulent effects become significant and require the introduction of eddy viscosity (η), which is not applicable in laminar scenarios. Thus, when flow transitions from laminar to turbulent, the factors affecting viscous flow calculations change drastically.
Consider pouring honey versus water. When you pour honey slowly, it moves smoothly (laminar flow), where only its viscosity plays a role. When the water is stirred rapidly, it starts to swirl and form eddies, and the internal forces change significantly (turbulent flow). In this way, the different viscosities give a practical understanding of laminar versus turbulent contexts.
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Eddy viscosity values depend on flow conditions and decrease towards the wall, reaching zero at the wall.
Eddy viscosity is dynamic and depends heavily on how the fluid interacts with surfaces as well as the overall flow pattern. As you approach the wall of a channel or pipe, the turbulence lessens due to the no-slip condition (the fluid at the wall has zero velocity), leading to a decrease in eddy viscosity until it is effectively zero at the boundary. Understanding this profile can help in designing more efficient fluid systems and predicting flows in various engineering contexts.
Imagine how rougher surfaces like gravel or a smooth surface like a sheet of glass affect how air flows over them. Near a smooth surface, air moves with less turbulence and fewer eddies compared to when it interacts with a gravelly surface, illustrating how physical boundaries can impact fluid behavior.
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Key Concepts
Turbulent Shear Stress: Defined as the sum of the viscous shear stress and the additional shear stress due to turbulence. It can be expressed as the product of eddy viscosity and the velocity gradient.
Eddy Viscosity: Unlike dynamic (μ) or kinematic viscosity (ν), eddy viscosity (η) is influenced by the turbulence in flow and becomes zero at the wall.
Reynolds Shear Stress: Introduced by Reynolds in 1886, which expresses turbulent shear stress as a function of fluctuating velocity components.
Prandtl’s Mixing Length Theory: This theory relates the turbulent shear stress to the average velocity gradient through a mixing length (l_m), which quantifies the distance at which fluid particles mix, leading to momentum transfer. Prandtl proposed that this mixing length is proportional to the distance from the wall (l_m = κ * y).
Understanding eddy viscosity and turbulent shear stress is critical for applications in hydraulic engineering and designing efficient systems for fluid flow processes.
See how the concepts apply in real-world scenarios to understand their practical implications.
Water flowing in a turbulent river where eddy viscosity significantly impacts flow rate measurements and structural design.
Airflow over an airplane wing where fluctuations create significant turbulence affecting lift and drag.
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In turbulent flow, the eddy's a friend, to measure shear stress, it helps us comprehend.
Imagine a river where fish swim layered; the mixing length is where their paths are paired, each layer flows, turbulence leads, all helping in the stream, as nature proceeds.
To remember Reynolds shear: 'Rushing Streams Have Effects’ — 'R' for Reynolds, 'S' for Shear, 'H' for hydrodynamics, 'E' for effects.
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Review the Definitions for terms.
Term: Eddy Viscosity
Definition:
A measure of the turbulent viscosity which is dependent on the flow conditions and contributes to shear stress in turbulent flows.
Term: Reynolds Shear Stress
Definition:
The turbulent shear stress resulting from the interaction of fluctuating velocity components in adjacent fluid layers.
Term: Mixing Length
Definition:
The distance over which fluid particles interact and mix, used to calculate turbulent shear stress.
Term: Boussinesq’s Model
Definition:
A model for expressing shear stress in turbulent flows that incorporates eddy viscosity.
Term: Dynamic Viscosity
Definition:
A measure of a fluid's resistance to shear flow, denoted by μ.