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Today we are diving deeper into the one-dimensional wave equation, which is fundamental in studying wave phenomena. Can anyone tell me what this wave equation looks like?
Is it \( \frac{\partial^2 u}{\partial t^2} = c^2 \frac{\partial^2 u}{\partial x^2} \)?
Exactly! That equation describes how the displacement of a wave depends on space and time. Now, who can explain what each term means?
The function \( u(x,t) \) gives the displacement, and \( c \) is the speed of the wave, right?
Spot on! This equation is crucial in understanding various types of waves. Now, let's explore how we can derive the solution.
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To derive D'Alembert’s solution, we will use a change of variables. Who remembers what those variables are?
Is it \( \xi = x + ct \) and \( \eta = x - ct \)?
Correct! Can you explain why we might want to make this change?
It simplifies the wave equation by separating the effects of time and position!
Exactly! By substituting these into our equation, we can express the second derivatives in a simpler form.
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Using our new variables, we find that our equation simplifies to \( \frac{\partial^2 u}{\partial \xi \partial \eta} = 0 \). What does this imply?
It suggests that \( u \) can be expressed as the sum of two functions, \( F(\xi) + G(\eta) \)!
Excellent! Now, how do we return to our original variables?
We just substitute back \( \xi \) and \( \eta \) back into the expression.
Precisely! This gives us D'Alembert's solution: \( u(x, t) = f(x + ct) + g(x - ct) \). Great job!
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Now, let's apply initial conditions to our solution. What are the initial conditions we usually work with?
We usually have the initial displacement \( u(x, 0) \) and the initial velocity \( \frac{\partial u}{\partial t} \).
Right! And from these, how do we relate them to functions \( f \) and \( g \)?
We plug in \( t = 0 \) into D'Alembert's solution to find \( f \) and \( g \).
Exactly! And once we do that, we can find our full solution accurately depicting the wave’s behavior. Make sure to communicate your solutions clearly!
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Today, we covered how to derive D'Alembert's solution to the one-dimensional wave equation. To summarize, what are the core pieces of knowledge we should hold onto?
We learned the formulation of the wave equation and how to transform it to find a solution.
The significance of using variables \( \xi \) and \( \eta \) to derive the general solution.
Absolutely! And recall that our full solution can incorporate initial conditions to tailor it to specific scenarios. Well done, everyone!
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In this section, the simplified partial differential equation (PDE) for the one-dimensional wave equation is analyzed through the derivation of D'Alembert's solution using change of variables, ultimately leading to an expression that describes how waveforms propagate.
In the study of wave motion, the one-dimensional wave equation
$$ \frac{\partial^2 u}{\partial t^2} = c^2 \frac{\partial^2 u}{\partial x^2} $$
is fundamental. The process of deriving D'Alembert’s solution begins by changing variables, introducing:
$$ \xi = x + ct, \eta = x - ct. $$
These new variables allow us to express the second derivatives in terms of these new coordinates. With these transformations, we can use the chain rule to simplify the equation into a form:
$$ \frac{\partial^2 u}{\partial \xi \partial \eta} = 0. $$
This indicates that the wave solutions can be represented as a sum of two functions of these variables:
$$ u = F(\xi) + G(\eta). $$
Returning to the original variables, we arrive at the classical solution:
$$ u(x,t) = f(x + ct) + g(x - ct), $$
where $f$ and $g$ are arbitrary twice-differentiable functions specifically chosen based on initial conditions. This foundational principle demonstrates the propagation of waveforms without distortion, laying the groundwork for numerous applications in physics and engineering.
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Given the equation from previous steps, we have the simplified form:
$$\frac{u}{\xi \eta} = 0$$
In this part, we start with the result obtained from the earlier manipulations of the wave equation. The key equation we look at now indicates that the second mixed partial derivative equals zero. This means that any wave solution can be expressed as a function that is separable with respect to two new variables: \(\xi\) and \(\eta\). So, we are going to solve the simplified partial differential equation (PDE) that we derived in the previous step.
Think of this like simplifying a puzzle. If you have many pieces that make a complicated picture, sometimes you can group similar pieces together to see the overall shape easier. Here, we are making the equation simpler to solve, just like grouping the puzzle pieces.
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The general solution of this PDE is represented as:
$$u(\xi, \eta) = F(\xi) + G(\eta)$$
From our statement that \(u = 0\) leads us to believe that the functions we are looking at can be expressed individually. This means that the overall behavior of the wave can be completely recovered by understanding two separate functions, \(F(\xi)\) and \(G(\eta)\). Each of these functions corresponds to waveforms traveling in opposite directions; \(F(\xi)\) is for one direction, while \(G(\eta)\) corresponds to the other.
Imagine you are at a busy intersection looking at traffic from two different roads. One road has cars moving straight towards you (let's say it's like \(F(\xi)\)), while cars from the other road are moving away from you. Each set of cars tells a different story of traffic flow, but together they provide a complete picture of what’s happening at the intersection.
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Finally, we return to our original variables to express the solution in the context of the wave equation:
$$u(x, t) = f(x + ct) + g(x - ct)$$
Once we have our general solution in the new variables, we need to transform it back to our original variables, which correspond to the physical quantities we're interested in. By substituting back the definitions of \(\xi\) and \(\eta\) in terms of the original variables \(x\) and \(t\), we recover the wave solution that can now be interpreted in a more concrete context—where the functions \(f\) and \(g\) represent waves propagating through space over time.
This is akin to translating a recipe from one language back to your native language. The recipe (solution) remains the same in terms of the ingredients, but it’s essential that it’s phrased in a way you understand so you can actually cook (apply the solution) using it.
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Key Concepts
One-Dimensional Wave Equation: Describes how waves propagate in one dimension using a second-order linear differential equation.
Change of Variables: A technique used to simplify equations by introducing new variables.
D'Alembert's Solution: The general solution to the wave equation given by the sum of two functions of \( \xi \) and \( \eta \).
See how the concepts apply in real-world scenarios to understand their practical implications.
The equation of a vibrating string can be modeled using the wave equation where it represents the displacement of the string over time.
In acoustics, sound waves propagating through air can also be described using the wave equation, allowing for understanding in applications like music.
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D'Alembert’s path we will not sever, waves travel left and right, forever!
Imagine a string tied to a wall. As you pluck it, it sends waves left and right, just like D'Alembert's solution, capturing its essence.
For remembering wave direction: 'Right and Left Anytime' (R.L.A.) for f(x + ct) and g(x - ct).
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Review the Definitions for terms.
Term: Wave Equation
Definition:
A second-order linear partial differential equation that describes the propagation of waves.
Term: D'Alembert's Solution
Definition:
A method for solving the one-dimensional wave equation expressed in terms of two arbitrary functions.
Term: Variables
Definition:
The terms \( \xi \) and \( \eta \) defined to simplify the wave equation.
Term: Initial Conditions
Definition:
The specified values for displacement and velocity used to solve the wave equation.