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Welcome class! Today, we are going to explore the dynamic free surface boundary condition. Can anyone tell me what a free surface is in fluid mechanics?
Isn't it the surface of the fluid that is open to the atmosphere, like the top of a lake?
That's right! The free surface is exposed and can distort due to various forces. Now, when we discuss boundary conditions for fluids, what do we think differentiates fixed surfaces from free surfaces?
Fixed surfaces resist pressure changes, whereas free surfaces can flow and distort?
Exactly! This leads us to the dynamic nature of free surfaces, which often requires unique equations and considerations in our calculations.
So, how does that affect the pressure on the free surface?
Good question! The pressure must be uniform across the free surface, as it cannot sustain variations. We'll derive the necessary equations later. Remember, 'pressure on the free surface is uniform' - a key point!
To understand how dynamic conditions affect our calculations, let’s look at kinematic boundary conditions. Can someone recall how we express these conditions mathematically?
Is it related to the rate of change of the free surface, like the displacement of the surface over time?
Right! We represent it using $F(x, y, z, t) = z - B{eta}(x, y, t)$. Now, we apply derivatives to find the change in the vertical flow velocities.
So what do we get from that application?
We'll find that $w = rac{ B{deta}}{ B{dt}} + u rac{ B{deta}}{ B{dx}} + v rac{ B{deta}}{ B{dy}}$ at $z = B{eta}$. This is crucial for surface motion.
Do we have to consider all flow directions here, including lateral?
Absolutely! As we calculate these variables, it helps us set a more complete understanding of wave motion.
Now, let's discuss the pressure distribution on our dynamic free surface. Why would a uniform pressure be needed?
Because it prevents distortions due to varying pressure that could create instability, right?
Spot on! We derive conditions based on this necessity. Are you familiar with the unsteady Bernoulli equation?
I remember it involves terms for kinetic and potential energy, but how does it relate here?
Great recall! It accommodates changes in our calculations, specifically at free surfaces. The pressure exerted must be uniform, as denoted in our derivations to assist stability.
Can we see how that links to boundary conditions?
Absolutely! We will apply this understanding practically as we prepare for lateral boundary conditions next.
Lastly, let’s talk about lateral boundary conditions. Can anyone define their significance in our models?
They help define how boundaries affect wave propagation in different spatial directions?
Exactly! Here, periodic boundary conditions may apply. For example, if waves in a channel do not change, we express that as $phi(x, t) = phi(x + L, t)$. So our conditions reset after a certain distance.
That helps in simplifying our calculations, doesn’t it?
Right! This periodicity is crucial, allowing us to analyze the flow effectively. Keep in mind, referring back to surface tension and wave characteristics also plays into this!
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The section discusses the implications of dynamic free surface boundary conditions, comparing them to fixed boundary conditions. It explains how pressure variations on a free surface come into play and how to apply them using kinematic equations, ultimately leading to the formula for pressure distribution along the free surface.
This section introduces the concept of dynamic free surface boundary conditions within the context of hydraulic engineering and wave mechanics. The free surface of a fluid allows for distortion, unlike fixed boundaries that can resist pressure variations. This dynamic nature requires special consideration when applying boundary conditions in fluid dynamics.
Initially, we establish that the boundary follows the equation $F(x, y, z, t) = z - B{eta}(x, y, t)$, defining the position of the free surface over time. From previous learning about boundary conditions, we derive a kinematic boundary condition as it pertains to dynamic systems. This leads to the formulation of $w = rac{ B{deta}}{ B{dt}} + u rac{ B{deta}}{ B{dx}} + v rac{ B{deta}}{ B{dy}}$ at the surface $z = B{eta}$, which encapsulates the relationship between the vertical velocity component at the surface and the horizontal velocities.
Additionally, we explore the need for a uniform pressure distribution along the water's surface in dynamic free surface problems, necessitated by the inability of free surfaces to support pressure differentials as effectively as fixed surfaces. An unsteady version of Bernoulli’s equation is employed to derive the dynamic profile of the free surface under various conditions, resulting in the final condition being dependent on both the wave properties and the curvature of the surface in cases of tension at the interface. Extensive notation assists in clarifying these advanced principles such as the pressure represented as $P_n$ and contributions from surface tension.
The section also introduces lateral boundary conditions and hints at the implications this has for wave propagation dynamics. This holistic approach strategically combines theoretical derivation with practical applications, putting emphasis on the real-world impact of wave mechanics in hydraulic engineering.
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Now, there is something called dynamic free surface boundary condition, free surface means, free surface of water is written as. So, you the surface is free it can distort if you recall from our open channel flow lectures.
The dynamic free surface boundary condition describes how the surface of water behaves when disturbed. Unlike a fixed boundary, a free surface can change or distort due to factors like waves or fluid motion. This means that the boundary at the surface is not constant and can rise or fall based on the fluid dynamics involved.
Think of a water balloon; when you poke it or push on it, the surface of the balloon changes shape. Similarly, the surface of water in a river or ocean changes shape due to waves or currents.
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So, if the surface is something like this, you know then the free surface and this is it as a function of x y and t, then we can write F of x y z, t = z – eta x y t.
To describe how the free surface of water fluctuates over time and space, we use a mathematical function, F(x,y,z,t). This function accounts for the vertical position (z) of any point on the surface, minus the water's free surface elevation (eta), which can vary based on location (x, y) and time (t). It essentially measures the distance from the free surface at any point.
Imagine tracking the height of ocean waves along a coastline. You can think of F as a way to measure how high the water rises and falls at each point along the shore throughout the day.
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So delta F is going to be delta F delta x i cap + delta F delta y Jacob + delta F delta z k cap, so, if we put F as here z - eta x y t, then we get – del eta del x – del eta del y + k cap.
In order to analyze the movement of the free surface, we calculate the change in F (ΔF) in all three spatial dimensions - x, y, and z. By substituting our earlier equation into this calculation, we can determine how the surface elevation changes relative to those dimensions, leading to rates of change for eta in both horizontal directions (x and y).
Imagine you're at a pool watching how water levels rise or fall at different spots. If someone jumps in or splashes, the waves will change at various places (x and y directions), and you'll have to observe how each point in the pool reacts at the same time (z direction).
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So, this is the equation of the free surface this is an important equation. So, this is the dynamic free surface boundary condition.
The derived dynamic free surface boundary condition is an essential equation that relates the water's surface velocity to its change over time. This equation incorporates not just the water motion along the surface but also how that motion is influenced by waves, ultimately describing how a free surface can dynamically change shape.
Think about a soccer player dribbling a ball on a wet grassy field. The way the ball moves across the surface (representing the water surface) can change rapidly, depending on how the player interacts with it (similar to how water reacts to wind or other forces).
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Therefore another boundary condition is required for any free surface or interface to prescribe the pressure distribution and the boundary. Since the free surface cannot support the pressure variation, we need to prescribe another boundary condition to tell what the pressure distribution on that particular boundary is and this is called the dynamic boundary condition.
Unlike fixed boundaries, where the pressure changes can be managed and calculated, free surfaces can only support uniform pressure along their length because they can deform. This requirement leads to the formation of additional boundary conditions to properly describe the pressure distribution atop a fluid's surface, known as dynamic boundary conditions.
Consider a trampoline; while jumping, the surface does not hold pressure variations well since it bends and shifts under weight. Instead, everyone on the trampoline experiences a roughly uniform bounce effect, akin to how water's free surface behaves under surface tension.
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To derive the dynamic free surface boundary condition we use unsteady Bernoulli’s equation on the free surface.
To accurately characterize the dynamics of the free surface, especially for fluids in motion, we apply Bernoulli's equation adjusted for changing conditions (unsteady), which helps illustrate how fluid pressure, velocity, and elevation interrelate at the free surface. This application forces us to consider both time and space changes, making the analysis richer and complex.
Imagine riding a roller coaster; your experience changes as you go up and down hills. Similarly, applying the unsteady Bernoulli equation helps us understand how the speed and pressure of the water changes as speed varies depending on surface waves.
Learn essential terms and foundational ideas that form the basis of the topic.
Key Concepts
Dynamic Free Surface: Defines the top boundary of a fluid that is free to distort.
Kinematic Boundary Condition: Describes how surface motion translates to fluid velocities.
Pressure Uniformity: The need for consistent pressure across fluid boundaries to maintain stability.
Bernoulli's Applicability: Use of Bernoulli's equation in deriving fluid motion equations in dynamic conditions.
Lateral Boundary Conditions: Considerations that affect flow dynamics from the sides of the fluid domain.
See how the concepts apply in real-world scenarios to understand their practical implications.
The behavior of ocean waves as they reflect movement on the free surface, showing the importance of dynamic conditions.
The application of Bernoulli's equation in predicting fluid speeds as water flows over a weir.
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When waves go up and down, the free surface is around, dynamic flow we can see, no pressure change to be!
Imagine the ocean's waves rolling under the sun. As they crest and fall, the water's surface dances freely, but can't change its pressure, resembling a well-choreographed fluid ballet.
DYNAMIC: Distinctive, Under Pressure, Needing Immediate Constant Assessment for movement!
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Review the Definitions for terms.
Term: Dynamic Free Surface
Definition:
The boundary of a fluid that is free to move and distort under the influence of external forces.
Term: Kinematic Boundary Condition
Definition:
A condition that relates the velocities of the fluid to the motion of the boundary surface.
Term: Surface Tension
Definition:
The elastic tendency of a fluid surface that makes it acquire the least surface area possible.
Term: Bernoulli's Equation
Definition:
A principle that describes the conservation of energy in flowing fluids, including potential and kinetic energy.
Term: Lateral Boundary Condition
Definition:
Conditions that apply at the sides of the fluid domain, affecting wave behavior and propagation.