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Show that the gravitational potential \(V=-G m / r\) satisfies Laplace's equation, that is, show that \(\nabla^{2}(1 / r)=0\) where \(r^{2}=x^{2}+y^{2}+z^{2}, r \neq 0\).

Short Answer

Expert verified
The potential \( V = \frac{1}{r} \) satisfies Laplace's equation, as its Laplacian is zero.

Step by step solution

01

Define the Gravitational Potential

The gravitational potential is given as \[V = -\frac{Gm}{r}\]. Here, \(G\) is the gravitational constant, \(m\) is the mass, and \(r\) is the distance from the mass point.
02

Express Laplace's Equation

Laplace's equation is given by \[abla^2 V = 0\]. To satisfy this equation, we need to find the Laplacian of our potential and show it equals zero.
03

Understand the Laplacian in Spherical Coordinates

Since the potential depends only on \(r\), we use spherical coordinates. In spherical coordinates, the Laplacian of a radially symmetric function \(f(r)\) is \[abla^2 f(r) = \frac{1}{r^2} \frac{d}{dr} \left( r^2 \frac{d f}{dr} \right)\].
04

Apply the Laplacian to the Given Potential

Substitute \(V = \frac{1}{r}\) into the spherical coordinates Laplacian formula: \[abla^2 \left( \frac{1}{r} \right) = \frac{1}{r^2} \frac{d}{dr} \left( r^2 \frac{d}{dr} \left( \frac{1}{r} \right) \right)\].
05

Compute the Derivatives

First, compute the first derivative: \[ \frac{d}{dr} \left( \frac{1}{r} \right) = -\frac{1}{r^2} \].Then compute the second derivative: \[ \frac{d}{dr} \left( -\frac{1}{r^2} \right) = \frac{2}{r^3} \].
06

Simplify the Expression

Substitute the second derivative back into the Laplacian formula: \[ abla^2 \left( \frac{1}{r} \right) = \frac{1}{r^2} \frac{d}{dr} \left( r^2 \left( -\frac{1}{r^2} \right) \right) = \frac{1}{r^2} \frac{d}{dr} (-1) = \frac{1}{r^2} \cdot 0 = 0\].
07

Conclude the Solution

Since the Laplacian of \( \frac{1}{r} \) is zero, \[abla^2 \left( \frac{1}{r} \right) = 0 \], it is proven that the gravitational potential satisfies Laplace's equation.

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Key Concepts

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

Laplace's Equation
Laplace's equation is a second-order partial differential equation. It is widely used in physics and engineering. The equation is: \[ abla^2 V = 0 \]. Here, \[ abla^2 \] (called the Laplacian) is the divergence of the gradient of a function. In simple terms, it measures how a function \(V\) deviates from its average value at a given point. Solutions to this equation, also known as harmonic functions, are important in fields like electrostatics, fluid dynamics, and gravitational potential theory.

In the context of gravitational potential, satisfying Laplace's equation implies that the potential \(V\) behaves in a manner consistent with the inverse-square law of gravitation.
Spherical Coordinates
Spherical coordinates are a system of coordinates that extends the concept of polar coordinates to three dimensions. They are especially useful for problems involving spherical symmetry. In spherical coordinates, any point in space is represented by three parameters: \[ (r, \theta, \phi) \], where \[ r \] is the radius or distance from the origin, \[ \theta \] is the angle in the \(xy\)-plane (similar to the polar angle), and \[ \phi \] is the angle from the \(z\)-axis (often called the azimuthal angle).

The notation uses:
  • \textbf{r}: distance from the origin
  • \textbf{θ}: angle in the \(xy\)-plane
  • \textbf{ \phi}: angle from the \(z\)-axis

For functions that only depend on \(r\), spherical coordinates simplify many calculations. This is especially true for problems with radial symmetry, like the gravitational potential.
Laplacian
The Laplacian, denoted \[ abla^2 \], is a differential operator that appears frequently in physics. It is defined as the sum of the second partial derivatives with respect to each spatial coordinate. In Cartesian coordinates, the Laplacian of a function \(V(x, y, z)\) is given by: \[ abla^2 V = \frac{abla^2 V}{abla x^2} + \frac{abla^2 V}{abla y^2} + \frac{abla^2 V}{abla z^2} \]

In spherical coordinates, if a function only depends on \(r\), the Laplacian is simplified to: \[ abla^2 V = \frac{1}{r^2} \frac{d}{dr}(r^2 \frac{dV}{dr}) \].

When you apply this to \(V = -Gm/r\), you first find the first and second derivatives of \(V\) with respect to \(r\). After that, substitute these derivatives back into the spherical coordinates form of the Laplacian. When these steps are done correctly, you'll see that \[ abla^2 V = 0 \], proving that Laplace's equation is satisfied.

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Most popular questions from this chapter

The Klein-Gordon equation is \(\nabla^{2} u=\left(1 / v^{2}\right) \partial^{2} u / \partial t^{2}+\lambda^{2} u .\) This equation is of interest in quantum mechanics, but it also has a simpler application. It describes, for example, the vibration of a stretched string which is embedded in an elastic medium. Separate the one-dimensional Klein-Gordon equation and find the characteristic frequencies of such a string.

A sphere initially at \(0^{\circ}\) has its surface kept at \(100^{\circ}\) from \(t=0\) on (for example, a frozen potato in boiling water!). Find the time- dependent temperature distribution. Hint: Subtract \(100^{\circ}\) from all temperatures and solve the problem; then add the \(100^{\circ}\) to the answer. Can you justify this procedure? Show that the Legendre function required for this problem is \(P_{0}\) and the \(r\) solution is \((1 / \sqrt{r}) J_{1 / 2}\) or \(j_{0}\) [see (17.4) in Chapter 12]. since spherical Bessel functions can be expressed in terms of elementary functions, the series in this problem can be thought of as either a Bessel series or a Fourier series. Show that the results are identical.

The following two \(R(r)\) equations arise in various separation of variables problems in polar, cylindrical, or spherical coordinates: $$\begin{aligned}&r \frac{d}{d r}\left(r \frac{d R}{d r}\right)=n^{2} R,\\\&\frac{d}{d r}\left(r^{2} \frac{d R}{d r}\right)=l(l+1) R.\end{aligned}$$ There are various ways of solving them: They are a standard kind of equation (often called Euler or Cauchy equations see Chapter \(8,\) Section \(7 \mathrm{d}\) ); you could use power series methods; given the fact that the solutions are just powers of \(r,\) it is easy to find the powers. Choose any method you like, and solve the two equations for future reference. Consider the case \(n=0\) separately. Is this necessary for \(l=0 ?\)

A long wire occupying the \(x\) axis is initially at rest. The end \(x=0\) is oscillated up and down so that $$ y(0, t)=2 \sin 3 t, \quad t >0 $$ Find the displacement \(y(x, t)\). The initial and boundary conditions are \(y(0, t)=\) \(2 \sin 3 t, y(x, 0)=0, \partial y /\left.\partial t\right|_{t=0}=0 .\) Take Laplace transforms of these conditions and of the wave equation with respect to \(t\) as in Example 1 . Solve the resulting differential equation to get $$ Y(x, p)=\frac{6 e^{-(p / v) x}}{p^{2}+9} $$Use \(L 3\) and \(L 28\) to find $$y(x, t)=\left\\{\begin{array}{cl} 2 \sin 3\left(t-\frac{x}{v}\right), & x < v t \\ 0, & x > v t \end{array}\right.$$

A square membrane of side \(l\) is distorted into the shape $$f(x, y)=x y(l-x)(l-y)$$ and released. Express its shape at subsequent times as an infinite series. Hint: Use a double Fourier series as in Problem \(5.9 .\)

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