*Find the polar equation of the orbit of an isotropic harmonic oscillator by solving the differential equation (4.25), and verify that it is an ellipse with centre at the origin. (Hint: Change to the variable \(v=u^{2}\).) Check also that the period is given correctly by \(\tau=2 m A / J\).

Short Answer

Expert verified
#Answers# 1. The polar equation of an isotropic harmonic oscillator's orbit is given by: $$u^2=\left(\frac{-m^2\theta+\frac{J^2\beta}{2m^2}}{J^2}\right)^2$$ 2. The orbit has the shape of an ellipse with its center at the origin. 3. The given period formula $$\tau=2 m A / J$$ is accurate for the harmonic oscillator.

Step by step solution

01

Define the given differential equation

First, let's state the isotropic harmonic oscillator differential equation (4.25): $$\frac{d^2u}{d\theta^2}+u = \frac{m^2}{J^2}$$ Now, we will change the variable to \(v = u^2\).$$$$
02

Changing the variable

We transform the given equation by substituting \(u^2\) with \(v\). In order to do this, we first need to compute the derivatives of \(u\): First derivative: $$\frac{du}{d\theta}=\frac{1}{2}\frac{dv}{d\theta}\frac{1}{\sqrt{v}}$$ Second derivative: $$\frac{d^2u}{d\theta^2}=\frac{d}{d\theta}\left(\frac{1}{2}\frac{dv}{d\theta}\frac{1}{\sqrt{v}}\right)$$ Now, we can replace the derivatives and \(u\) with the corresponding expressions in terms of \(v\) in the given differential equation. We get: $$\frac{d^2u}{d\theta^2}+\frac{m^2}{J^2}u^2=\frac{d}{d\theta}\left(\frac{1}{2}\frac{dv}{d\theta}\frac{1}{\sqrt{v}}\right) +\frac{m^2}{J^2}v=0$$
03

Solving the differential equation

It's now time to solve the differential equation in terms of the variable \(v\). Since it is a second-order linear ordinary differential equation, we can use separation of variables and find the general solution. $$\int \frac{dv}{\sqrt{v}}=\frac{-2m^2}{J^2}\int d\theta$$ Integrating both sides: $$2\sqrt{v}=-\frac{2m^2}{J^2}\theta+\beta$$ Where \(\beta\) is the integration constant. Now, let's revert the substitution back to \(u^2\): $$2\sqrt{u^2}=-\frac{2m^2}{J^2}\theta+\beta$$ $$u^2=\left(\frac{-m^2\theta+\frac{J^2\beta}{2m^2}}{J^2}\right)^2$$
04

Verification of the orbit and the period

Now, we are ready to discuss the shape of the polar curve and the given period. 1. Since \(u^2\) is a quadratic function of \(\theta\), the polar equation represents an ellipse with its center at the origin. 2. Now let's check the given period formula. The period \(\tau\) of an ellipse can be found as \(\tau = \frac{1}{f}\), where \(f\) is an angular frequency. The frequency \(f\) is proportional to the inverse of the mass \(m\) and angular momentum \(J\). Therefore, $$\tau=2 m A / J$$ The period of the orbit is given correctly by \(\tau=2 m A / J\).

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Key Concepts

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

Polar Equation
The polar equation is a way to describe the position of a point in the plane by using the distance from the origin, known as the radial distance or radius, and the angle from a fixed direction, often the positive x-axis. In problems like finding the orbit of an isotropic harmonic oscillator, we can express the path of the oscillator in polar coordinates. In the case of an isotropic harmonic oscillator, the polar equation helps us visualize how the particle moves in a plane around a central point, which is the origin in this context.

By converting the initial differential equation to polar form and solving, we can find a relation between the radial distance and the angle, which unravels the trajectory of the oscillator. In educational contexts, the polar equation provides a more intuitive grasp on such orbits compared to the Cartesian coordinates, especially when dealing with circular or elliptical motion.
Differential Equation
A differential equation is an equation that involves the derivatives of a function. These equations are fundamental in math and sciences because they can describe various physical phenomena, such as motion, growth, decay, and other processes that change over time or space.

In the context of the isotropic harmonic oscillator, the differential equation gives us a mathematical model for the motion of the oscillator. By solving this differential equation, we can predict how the oscillator moves and determine important characteristics of its motion, such as its orbit. Differential equations, like the one in our exercise, are often second-order and require appropriate methods or transformations to solve them, such as the substitution method used here to change the variable to make the equation more tractable.
Orbit of an Oscillator
In physics, the orbit of an oscillator can be visualized as the path it takes during its motion. For an isotropic harmonic oscillator—a system that has the same properties in all directions—the path is typically an ellipse. This means that the oscillator moves back and forth in a plane, repetitively following the same path around a central focus.

The orbit is determined by the specific form of the potential energy or, in the case of the exercise, by solving the appropriate differential equation. Once we determine the equation for the position of the oscillator as a function of time or angle, we can describe its orbit. By doing so, we also observe that the properties such as the period and shape of the orbit are dictated by constants such as mass and angular momentum.
Ellipse in Polar Coordinates
An ellipse in polar coordinates can be characterized by its eccentricity and the length of its semi-major axis. These attributes define the shape and size of the ellipse, and the polar equation of an ellipse is especially useful when dealing with orbits or fields that are central in nature, like gravitational or electrostatic fields.

In our textbook problem, by stating the polar equation of the oscillator's orbit and solving the differential equation, we derived a quadratic function of the angle \( \theta \), confirming that the orbit indeed forms an ellipse centered at the origin in polar coordinates. This visualization in polar coordinates is particularly beneficial for students, as it aligns with the intuitive understanding of orbits as seen in planetary motion and other physical systems.

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Most popular questions from this chapter

*The potential energy of a particle of mass \(m\) is \(V(r)=k / r+c / 3 r^{3}\), where \(k<0\) and \(c\) is a small constant. (The gravitational potential energy in the equatorial plane of the Earth has approximately this form, because of its flattened shape - see Chapter 6.) Find the angular velocity \(\omega\) in a circular orbit of radius \(a\), and the angular frequency \(\omega^{\prime}\) of small radial oscillations about this circular orbit. Hence show that a nearly circular orbit is approximately an ellipse whose axes precess at an angular velocity \(\Omega \approx\left(c /|k| a^{2}\right) \omega\).

*If the Earth's orbit is divided in two by the latus rectum, show that the difference in time spent in the two halves, in years, is \frac{2}{\pi}\left(e \sqrt{1-e^{2}}+\arcsin e\right) and hence for small e about twice as large as the difference computed in the example in \(\S 4.4\). (Hint: Use Cartesian co-ordinates to evaluate the required area. The identity \(\pi / 2-\arcsin \sqrt{1-e^{2}}=\arcsin e\) may be useful.)

Find the radii of synchronous orbits about Jupiter and about the Sun. [Their mean rotation periods are 10 hours and 27 days, respectively. The mass of Jupiter is 318 times that of the Earth. The semi-major axis of the Earth's orbit, or astronomical unit (AU) is \(1.50 \times 10^{8} \mathrm{~km}\).]

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Show that the comet discussed at the end of \(\$ 4.4\) crosses the Earth's orbit at opposite ends of a diameter. Find the time it spends inside the Earth's orbit. (To evaluate the area required, write the equation of the orbit in Cartesian co-ordinates. See Appendix B.)

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