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Today, we'll discuss the concept of bottom boundary conditions, which are crucial in fluid mechanics. Can anyone tell me what they think happens at the bottom of a fluid surface?
Well, I think the bottom is where the fluid doesn't move?
Exactly! At the bottom boundary, we often determine that the velocity normal to the boundary is zero, denoted as u·n = 0. This leads us to the equation z = -h(x). Why do you think we write it this way?
Is it because we want to define the surface in terms of depth?
Correct! This gives us insight into how we model our surfaces based on fluid height. Always remember, H2O at rest has a fixed bottom boundary. Let's move on.
Now that we understand our surface, let’s derive the relationships for velocities at the bottom boundary. When u is the x-directional velocity and w is the z-directional velocity, what expressions do we use?
We’ve learned in previous sessions that w = - u * (dh/dx)?
Correct again! This equation helps us establish a relationship between the flow and the slope of the bottom. If it was a flat surface, what would happen to w?
W would be zero in that case!
Absolutely! No slope means no vertical flow. Thus, we see the importance of how the surface slopes affect fluid behavior.
Let’s shift focus to dynamic free surface boundary conditions. Why do we need another condition when considering pressure distribution?
Because the surface can distort and doesn’t support pressure variations like fixed surfaces do?
Exactly! The pressure on the free surface needs to be uniform along the wave form. We use unsteady Bernoulli’s equation to derive this relationship. Can someone summarize this equation for me?
Isn't it like an adjustment to the Bernoulli's equation that includes time as a variable?
Exactly right! Incorporating time dynamics allows us to consider faster changes in the system, which is critical for understanding wave motion.
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The section presents the unsteady Bernoulli's equation, focusing on its derivation and application to dynamic free surface boundary conditions. The discussion includes various boundary conditions, including bottom and free surface conditions, along with examples illustrating the concepts.
This section delves into the unsteady Bernoulli’s equation, a vital tool in hydraulic engineering. We start by reviewing the bottom boundary conditions (BBC) and how to relate them to the general flow of water. We establish that the function describing the surface can be expressed as z = - h(x). When analyzing the bottom boundary conditions, we see that under fixed conditions, the velocity normal to the boundary must be zero.
Applying this, we derive the x and z directional velocities at the bottom boundary. Transitioning to a general case, when the bottom is sloped, we simplify our findings to the relationship w/u = - dh/dx, allowing us to treat the bottom as a streamline based on the flow characteristics.
We subsequently discuss dynamic free surface boundary conditions, where the pressure distribution along the free surface requires the unsteady Bernoulli's equation considering pressure variations. The section emphasizes the influence of curvature at the free surface and its interaction with surface tension in determining pressure states.
Examples, exercises, and narrative dialogues reinforce these concepts, underscoring the importance of understanding the principles underlying free surface phenomena in fluid flows.
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Dynamic free surface boundary condition requires that the pressure on the free surface be uniform along the waveform. To derive this, we will use unsteady Bernoulli’s equation. This means that we will add another term to the standard Bernoulli’s equation to account for time variations.
The dynamic free surface boundary condition is vital in fluid mechanics because it acknowledges that pressure varies across a surface which can deform, such as the surface of water in a wave. By using the unsteady Bernoulli’s equation, we can express the relationship between fluid velocity, pressure, and elevation at that surface. The additional term makes the equation account for changes over time, reflecting how pressure is distributed over such dynamic surfaces.
Think of the ocean surface during a storm. As waves rise and fall, we can't simply assume the pressure above the water is constant; it fluctuates based on the wave height and speed. By using the dynamic free surface boundary condition, we can better understand and predict phenomena like the force of waves on a shore.
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To derive the dynamic boundary condition, we assume the gauge pressure Pn is 0. If the wavelength is very short, we have to consider the importance of surface tension, leading to equations where curvature at the water's surface affects pressure distribution.
When deriving the dynamic boundary condition using unsteady Bernoulli’s equation, we simplify by assuming that gauge pressure is zero at the surface. In scenarios where wavelengths are short, surface tension becomes significant, impacting the pressure at the water surface. This leads us to express how pressure variations occur due to curvature at the water surface, providing insights into wave dynamics.
Imagine blowing bubbles into a drink; the surface tension creates a curved shape at the surface of the bubble, which results in different pressure readings at the bubble’s edge compared to the flat surface of the drink. This principle can also explain how raindrops form; they resist deformation due to surface tension, just like waves resist flattening.
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In analyzing the water surface under wave motion, we can derive that the pressure beneath the free surface (P) is affected by the curvature (represented by surface tension) leading to representation where P is expressed as Pn - σ (d²η/dx²), linking pressure variation to wave curvature.
When looking at fluid dynamics with waves, the shape of the surface impacts the underlying pressure. The formula indicates this relationship—taking into account the curvature represents how waves distort the regular flow pattern, affecting pressure distribution underneath. This is crucial for understanding how waves carry energy and momentum.
Consider how a basketball appears as it bounces on the court. As it hits the ground, the shape curvature alters and creates pressure that helps it bounce back. Similarly, in waves, the curvature at the peaks alters the pressure beneath, influencing how the wave propagates.
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Key Concepts
Bernoulli’s Principle: A principle stating that an increase in the speed of a fluid occurs simultaneously with a decrease in pressure or potential energy.
Boundary Conditions: Constraints applied at the boundaries of a fluid flow, essential for solving fluid mechanics problems.
Dynamic Free Surface: A fluid's surface that can deform and affect pressure and flow dynamics.
See how the concepts apply in real-world scenarios to understand their practical implications.
In a scenario where a river’s flow height is adjustable, the application of unsteady Bernoulli's equation helps us analyze the changes in water pressure and flow velocity over time.
When a wave crashes onto a shoreline, the dynamic characteristics of the free surface become crucial for predicting erosion patterns influenced by wave pressure.
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When water flows, it knows the rules, at surfaces fixed, it won’t play fool.
Imagine a river with a steep bank; it rushes past, not breaking rank. But on the flat, slow it must stay, for on steady ground it cannot sway.
Bernoulli's Unsteady: BUB - Boundary, Unsteady, and Balance for understanding forces!
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Review the Definitions for terms.
Term: Boundary Condition
Definition:
Constraints necessary for solving differential equations representing physical systems, typically applied at the surfaces or boundaries.
Term: Dynamic Free Surface
Definition:
A fluid surface that can deform freely, influenced by various forces, unlike fixed surfaces that resist pressure changes.
Term: Unsteady Bernoulli’s Equation
Definition:
An extension of Bernoulli’s principle which incorporates time variations in flow characteristics.