Chapter 13: Problem 36
A solid is described along with its density function. Find the center of mass of the solid using spherical coordinates. (Note: these are the same solids and density functions as found in Exercises 31 through \(34 .)\) The spherical shell bounded between \(x^{2}+y^{2}+z^{2}=16\) and \(x^{2}+y^{2}+z^{2}=25\) with density function \(\delta(x, y, z)=\) \(\sqrt{x^{2}+y^{2}+z^{2}}\)
Short Answer
Step by step solution
Convert to Spherical Coordinates
Express Density Function
Formula for Mass and Integrals
Compute Mass Integral
Compute Moments for Center of Mass
Center of Mass Calculation
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Key Concepts
These are the key concepts you need to understand to accurately answer the question.
Spherical Coordinates
Here's a quick breakdown of these parameters:
- \( \rho \) is the radial distance from the origin to the point.
- \( \phi \) (or polar angle) is the angle from the positive z-axis.
- \( \theta \) (or azimuthal angle) is the angle in the x-y plane from the positive x-axis.
- \( x = \rho \sin\phi \cos\theta \)
- \( y = \rho \sin\phi \sin\theta \)
- \( z = \rho \cos\phi \)
Density Function
In spherical coordinates, this function simplifies beautifully to \( \rho \). This simplification occurs because:
- The Cartesian expression \( \sqrt{x^{2} + y^{2} + z^{2}} \) directly corresponds to the distance from the origin, precisely what \( \rho \) measures.
Mass Integral
The formula for the mass \( M \) is given by:\[ M = \int_0^{2\pi} \int_0^{\pi} \int_4^5 \rho^3 \sin\phi \, d\rho \, d\phi \, d\theta \]
This formula is derived from:
- \( \rho^2 \) as a substitution for the volume element of a sphere in spherical coordinates.
- Multiplying by \( \rho \) because it serves as the density function.
Moments Calculation
Here's a simple overview of moments:
- Moment about the yz-plane is denoted \( Mx \).
- Moment about the xz-plane is denoted \( My \).
- Moment about the xy-plane is denoted \( Mz \).
Because of symmetry for a full spherical shell, these moments often simplify. The integrals yield zero for the x and y components due to their corresponding cosine and sine functions integrating to zero over a complete periodic interval. Thus, these computations ultimately provide coordinates for the center of mass.