/*! This file is auto-generated */ .wp-block-button__link{color:#fff;background-color:#32373c;border-radius:9999px;box-shadow:none;text-decoration:none;padding:calc(.667em + 2px) calc(1.333em + 2px);font-size:1.125em}.wp-block-file__button{background:#32373c;color:#fff;text-decoration:none} Problem 20 Consider a square pulse \(\psi(t... [FREE SOLUTION] | 91Ó°ÊÓ

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Consider a square pulse \(\psi(t)\) which is zero for all \(t\) not in the interval \(t_{1}\) to \(t_{2}\). Within that interval, \(\psi(t)\) has the constant value \(1 / \Delta t\), where \(\Delta t=t_{2}-t_{1}\). Let \(t_{0}\) be the time at the center of the interval. Show that \(\psi(t)\) can be Fourier-analyzed as follows: $$ \psi(t)=\int_{0}^{\infty} A(\omega) \sin \omega\left(t-t_{0}\right) d \omega+\int_{0}^{\infty} B(\omega) \cos \omega\left(t-t_{0}\right) d \omega, $$ with the solution $$ A(\omega)=0, \quad B(\omega)=\frac{1}{\pi} \frac{\sin \frac{1}{2} \Delta t \omega}{\frac{1}{2} \Delta t \omega} $$ Sketch \(B(\omega)\) versus \(\omega .\) In the limit where \(\Delta t\) goes to zero, \(\psi(t)\) is called'a "delta function" of time, written \(\rho\left(t-t_{0}\right) .\) What is \(B(\omega)\) for this delta function of time?

Short Answer

Expert verified
B(ω) for the delta function is 1.

Step by step solution

01

Define the Square Pulse Function

The given function \( \psi(t) \) is defined as zero for all \( t \) not in the interval \( t_1 \) to \( t_2 \) and equal to \( \frac{1}{\Delta t} \) in this interval, where \( \Delta t = t_2 - t_1 \). Thus,\[\psi(t) = \begin{cases} \frac{1}{\Delta t}, & t_1 \leq t \leq t_2 \0, & \text{otherwise}\end{cases}\]
02

Apply Fourier Sine and Cosine Transforms

The problem statement gives a Fourier representation of \( \psi(t) \) as follows:\[\psi(t)=\int_{0}^{\infty} A(\omega) \sin \omega\left(t-t_{0}\right) d \omega + \int_{0}^{\infty} B(\omega) \cos \omega\left(t-t_{0}\right) d \omega.\]Given that \( A(\omega) = 0 \), we only need to find the function \( B(\omega) \).
03

Derive the Coefficient B(ω)

To find \( B(\omega) \), compute the cosine transform of the square pulse:\[B(\omega) = \frac{2}{\pi} \int_{t_1}^{t_2} \psi(t) \cos \omega(t - t_0) dt.\]Substituting \( \psi(t) = \frac{1}{\Delta t} \) and the integration limits, we have:\[B(\omega) = \frac{2}{\pi \Delta t} \int_{t_1}^{t_2} \cos \omega(t - t_0) dt.\]
04

Calculate the Integral

Change the variable of integration to simplify the expression: let \( x = \omega(t - t_0) \), then \( dx = \omega dt \). The integral becomes:\[B(\omega) = \frac{2}{\pi \Delta t \omega} \left[ \sin \omega(t - t_0) \right]_{t_1}^{t_2}.\]Evaluating, we find:\[B(\omega) = \frac{2}{\pi \Delta t \omega} \left( \sin \omega(t_2 - t_0) - \sin \omega(t_1 - t_0) \right).\]
05

Simplify the Expression for B(ω)

Express \( \sin(\text{difference of angles}) \) using the sine subtraction identity:\[\sin c - \sin d = 2 \cos \left(\frac{c + d}{2}\right) \sin \left(\frac{c - d}{2}\right).\]This simplifies \( B(\omega) \) to:\[B(\omega) = \frac{1}{\pi} \frac{\sin \frac{1}{2} \Delta t \omega}{\frac{1}{2} \Delta t \omega}.\]
06

Analyze the Limit for Delta Function and Sketch

In the limit \( \Delta t \to 0 \), \( \psi(t) \) becomes a delta function \( \rho(t - t_0) \). For this delta function, the limit of \( B(\omega) \) is:\[B(\omega) = 1.\]On a graph, \( B(\omega) \) versus \( \omega \) is a sinc function given by the equation in Step 5, which converges to 1 as \( \Delta t \to 0 \).

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Square Pulse Function
A square pulse function is a simplistic model often used in signal processing and Fourier analysis. In the context of a square pulse, consider a time interval between \( t_1 \) and \( t_2 \). Within this interval, a signal maintains a constant value, while outside this interval it is zero.

The expression for a square pulse \( \psi(t) \) can be written as:
  • \( \psi(t) = \frac{1}{\Delta t} \) for \( t_1 \leq t \leq t_2 \)
  • \( \psi(t) = 0 \) otherwise
The term \( \Delta t = t_2 - t_1 \) defines the width of the pulse, and the choice of \( \frac{1}{\Delta t} \) ensures that the integral of the pulse function over the interval is one. This normalization reflects the energy content of the signal being one unit, a typical requirement in signal processing.
Delta Function
The delta function, often referred to as Dirac's delta function, is an idealized concept in mathematics and signal processing that serves as a useful tool in various analyses, including Fourier analysis. As \( \Delta t \) approaches zero in the square pulse function, its behavior models that of a delta function.

The delta function has the property:
  • \( \rho(t-t_0) = 0 \) for \( t eq t_0 \)
  • The integral over the entire real line is 1: \( \int_{-\infty}^{\infty} \rho(t-t_0)dt = 1 \)
In the context of Fourier analysis, as the pulse width \( \Delta t \) compresses to zero, the spectrum \( B(\omega) \) converges to a constant value of 1, suggesting a flat frequency response. This reflects the delta function's property of containing all frequencies equally.
Cosine Transform
The cosine transform is a mathematical tool used in the analysis and computation of waveforms. It's part of the Fourier transform framework where functions or signals are expressed as a sum of cosine functions of different frequencies.

In our exercise, the square pulse is expanded using a cosine transform, recognizing that \( A(\omega) = 0 \). Therefore, we focus on:
  • \( B(\omega) = \frac{1}{\pi} \frac{\sin \frac{1}{2} \Delta t \omega}{\frac{1}{2} \Delta t \omega} \)
This expression is derived by computing the cosine Fourier transform of the square pulse, and it highlights the use of the cosine basis to represent signals in terms of frequencies. This approach facilitates the decomposition of the square pulse into basic harmonic components, each characterized by a cosine function with an associated amplitude \( B(\omega) \).
Sinc Function
The sinc function is a mathematical function that arises frequently in signal processing, especially in Fourier analysis. It is defined as \( \text{sinc}(x) = \frac{\sin(\pi x)}{\pi x} \), except at \( x = 0 \), where \( \text{sinc}(0) = 1 \).

In our exercise, \( B(\omega) \) is expressed in terms of a sinc function:
  • \( B(\omega) = \frac{1}{\pi} \frac{\sin \frac{1}{2} \Delta t \omega}{\frac{1}{2} \Delta t \omega} \)
This form of \( B(\omega) \) reveals that it assumes the shape of a sinc function with respect to frequency \( \omega \).
The sinc function has a pivotal role because it describes how the amplitude of each frequency component decays from the peak at zero frequency. The central peak extends to lower frequencies, with side lobes decaying steadily, exhibiting symmetry about the vertical axis. This characteristic captures the frequency response of the square pulse and explains the oscillating nature of its spectrum.

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Most popular questions from this chapter

Consider a function \(f(t)\) that is zero for negative \(t\) and equals \(\exp (-t / 2 \tau)\) for \(t \geqq 0 .\) Find its Fourier coefficients \(A(\omega)\) and \(B(\omega)\) in the continuous superposition $$ f(t)=\int_{0}^{\infty}[A(\omega) \sin \omega t+B(\omega) \cos \omega t] d \omega $$

Show that the sum of two traveling harmonic waves \(A_{1} \cos \left(\omega t-k z+\varphi_{1}\right)\) and \(A_{2} \cos \left(\omega t-k z+\varphi_{2}\right)\) traveling in the \(+z\) direction and having the same frequency \(\omega\) is itself a harmonic traveling wave of the same kind. That is, the sum can be written in the form \(A \cos (\omega t-k z+\varphi)\). Find out how \(A\) and \(\varphi\) are related to \(A_{1}, A_{2}\), \(\varphi_{1}\), and \(\varphi_{2} .\) (Hint: The use of complex numbers or a rotating vector diagram helps immensely.)

This experiment requires a piano. Trill two adjacent notes (a halftone apart). First pick two notes near the top of the keyboard. Trill slowly, then as fast as you can. Estimate the trill frequency. Can you still easily make out the two notes of the trill? Now trill two adjacent notes near the bottom of the keyboard, first very slowly, then gradually more rapidly. Is there a speed at which the two notes blend into a messy, indistinguishable mixture? Estimate the frequency where things get messy. Then do arithmetic and decide how good your ear and brain are at recognizing two separate maxima in the Fourier analysis, even when the frequency widths of the peaks (at balf-maximum intensity) are not small compared to the frequency spacing between the maxima.

The best way to understand the difference between phase and group velocities is to make water wave packets. To make expanding circular wave packets having dominant wavelength 3 or \(4 \mathrm{~cm}\) or longer, throw a big rock in a pond or pool. To make straight waves (the two-dimensional analog of threedimensional plane waves) with wavelengths of several centimeters, float a stick across the end of a bathtub or a large pan of water. Give the stick about two swift vertical pushes with your hand. After some practice, you should see that for these packets the phase velocity is greater than the group velocity. (See Table \(6.1\), Sec. 6.2.) You will see little wavelets grow from zero at the rear end of the packet, travel through the packet, and disappear at the front. (It takes practice; the waves travel rather fast.) Another good method is to put a board at the end of a bathtub and tap the board. To make millimeter-wavelength waves (surface tension waves), use an eyedropper full of water. Squeeze out one drop and let it fall on your pan or tub of water. First let the drop fall from a height of only a few millimeters. This gives dominant wavelengths of only a few millimeters. To see that these waves really are due to surface tension, add some soap to the water and repeat the experiment. You should notice a decrease in the group velocity when you add the soap. (To see that the longer wavelength waves are not due to surface tension, you can repeat the experiment at long wavelengths.) To lengthen the dominant wavelength of the group, let the water drop fall from a greater height. Here is a way to see (without doing a difficult measurement) that millimeter waves have a faster group velocity than waves of a centimeter or so. Generate a packet that has both millimeter and centimeter waves by dropping a water drop from a height of a foot or 50 into a circular pan filled to the brim. (A coffee can works very well.) Drop the drop near the center of the circular pan. Notice that after reflection from the rim the group comes to a focus at a point that is conjugate to the point where the drop hit. (By two conjugate points we mean points located on a line through the center of the circle and lying at equal distances on either side of the center.) When the packet is passing through the conjugate focus, there is a transitory standing wave there (similar to the transitory standing wave you get when you shake a wave packet onto a slinky tied to a wall). This enables you to judge the average arrival time of the packet. Look to see if there is a difference in arrival times for short- wavelength contributions to the packet as compared with longer wavelength contributions. It is difficult to measure, but you can see the effect fairly easily. An experiment \(I\) have not yet tried is to find a smooth running stream with flow velocity roughly equal to the group velocity for reasonable wavelengths. One should be able to make wave packets that travel upstream at about the flow velocity, so that the packet remains nearly at rest in your reference frame (assuming you are wading, not floating with the current). Surely that would be a most pleasant way to study wave packets.

Show that for light of index \(n(\lambda)\), $$ \frac{1}{v_{g}}=\frac{1}{v_{\varphi}}-\frac{1}{c} \lambda \frac{d n(\lambda)}{d \bar{\lambda}} $$ where \(\lambda\) is the vacuum wavelength of the light.

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